http://coloradoriverscience.org/index.php?action=history&feed=atom&title=Salinity 2026-07-25T16:32:48Z Revision history for this page on the wiki MediaWiki 1.43.0 http://coloradoriverscience.org/index.php?title=Salinity&diff=3573&oldid=prev 2023-10-18T21:26:09Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 17:26, 18 October 2023</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l5">Line 5:</td> <td colspan="2" class="diff-lineno">Line 5:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Following protests <del style="font-weight: bold; text-decoration: none;">in </del>Mexico about the excessive salinity of the Colorado River water deliveries <del style="font-weight: bold; text-decoration: none;">to Mexico </del>and implicit violations of the 1944 US-Mexico Water Treaty, <del style="font-weight: bold; text-decoration: none;">salinity control measures were established across </del>the <del style="font-weight: bold; text-decoration: none;">Colorado River Basin. The </del>Colorado River Basin Salinity Control Act (1973) established salinity criteria at three monitoring locations along the River and required the implementation of salinity control programs. The monitoring locations and target salinity concentrations are: below Hoover Dam (723 mg/L), below Parker Dam (747 mg/L), and at Imperial Dam (879 mg/L).</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>Following protests <ins style="font-weight: bold; text-decoration: none;">by </ins>Mexico about the excessive salinity of the Colorado River water deliveries and implicit violations of the 1944 US-Mexico Water Treaty, the Colorado River Basin Salinity Control Act (1973) established salinity criteria at three monitoring locations along the River and required the implementation of salinity control programs. The monitoring locations and target salinity concentrations are: below Hoover Dam (723 mg/L), below Parker Dam (747 mg/L), and at Imperial Dam (879 mg/L).</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The salinity control programs include salinity control units at Paradox Valley (CO), Grand Valley (CO), Las Vegas Wash (NV), and Crystal Geyser (UT) in addition to voluntary on-farm salinity control programs. Salinity control measures were estimated to control 1.22 million tons of salt annually in 2020 (about 10-12% of the salinity measured below Hoover Dam). Minute No. 242 mandates that the salinity of water deliveries to Mexico upstream of the Morelos Dam be no more than 115 ± 30 mg/L above average annual flow-weighted salinity of the Colorado River arriving at Imperial Dam.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Salinity is the only water quality issue that Reclamation is obligated to monitor and address at the basin scale; Reclamation spends approximately $35 million annually on salinity measures. </ins>The salinity control programs include salinity control units at Paradox Valley (CO), Grand Valley (CO), Las Vegas Wash (NV), and Crystal Geyser (UT) in addition to voluntary on-farm salinity control programs. Salinity control measures were estimated to control 1.22 million tons of salt annually in 2020 (about 10-12% of the salinity measured below Hoover Dam). Minute No. 242 mandates that the salinity of water deliveries to Mexico upstream of the Morelos Dam be no more than 115 ± 30 mg/L above average annual flow-weighted salinity of the Colorado River arriving at Imperial Dam.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">==Relevance==</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Even with </ins>the <ins style="font-weight: bold; text-decoration: none;">salinity control program in place, </ins>and <ins style="font-weight: bold; text-decoration: none;">consequent declines in </ins>salinity<ins style="font-weight: bold; text-decoration: none;">, </ins>Reclamation <ins style="font-weight: bold; text-decoration: none;">estimates </ins>that high salinity in the <ins style="font-weight: bold; text-decoration: none;">river still </ins>causes $300-400 million in economic damages annually. Roughly half of these economic impacts occur in the agricultural sector, as many high-value crops are sensitive to high salinity. Other impacts include pipe corrosion and higher costs of water treatment.  </div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">Salinity is </del>the <del style="font-weight: bold; text-decoration: none;">only water quality issue the Bureau of Reclamation is obligated to monitor </del>and <del style="font-weight: bold; text-decoration: none;">address at the basin-scale; Reclamation spends approximately $35 million annually on </del>salinity <del style="font-weight: bold; text-decoration: none;">measures. The Bureau of </del>Reclamation <del style="font-weight: bold; text-decoration: none;">estimated in 2017 </del>that high salinity in the <del style="font-weight: bold; text-decoration: none;">Colorado River </del>causes $300-<del style="font-weight: bold; text-decoration: none;">$</del>400 million in economic damages annually. Roughly half of these economic impacts occur in the agricultural sector, as many high-value crops are sensitive to high salinity. Other impacts include pipe corrosion and higher costs of water treatment<del style="font-weight: bold; text-decoration: none;">. Rising salinity in the Salton Sea (CA) has deleterious effects on agriculture, human health, environmental health, and local economies</del>.</div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Data and Tools==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Data and Tools==</div></td></tr> </table>

JeffreyJLukas http://coloradoriverscience.org/index.php?title=Salinity&diff=3173&oldid=prev 2022-12-02T15:01:15Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:01, 2 December 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l30">Line 30:</td> <td colspan="2" class="diff-lineno">Line 30:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Substantial Declines in Salinity Observed Across the Upper Colorado River Basin During the 20th Century, 1929–2019 (Rumsey et al. 2021).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Substantial Declines in Salinity Observed Across the Upper Colorado River Basin During the 20th Century, 1929–2019 (Rumsey et al. 2021).</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[https://www.coloradoriversalinity.org/docs/2020WR028581.pdf<del style="font-weight: bold; text-decoration: none;">/ </del>Rumsey et al., 2021]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[https://www.coloradoriversalinity.org/docs/2020WR028581.pdf Rumsey et al., 2021]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[https://www.usbr.gov/projects/pdf.php?id=96/ Colorado River Basin Salinity Control Project]</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>[https://www.usbr.gov/projects/pdf.php?id=96/ Colorado River Basin Salinity Control Project]</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=3109&oldid=prev 2022-11-29T15:14:44Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:14, 29 November 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l23">Line 23:</td> <td colspan="2" class="diff-lineno">Line 23:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  https://doi.org/10.3133/sir20175009 <del style="font-weight: bold; text-decoration: none;">/ </del>upper Colorado River Basin salinity]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  <ins style="font-weight: bold; text-decoration: none;">[</ins>https://doi.org/10.3133/sir20175009 upper Colorado River Basin salinity]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=3108&oldid=prev 2022-11-29T15:13:44Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:13, 29 November 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l23">Line 23:</td> <td colspan="2" class="diff-lineno">Line 23:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  https://doi.org/10.3133/sir20175009/ upper Colorado River Basin salinity]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  https://doi.org/10.3133/sir20175009 / upper Colorado River Basin salinity]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=3107&oldid=prev 2022-11-29T15:13:08Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:13, 29 November 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l23">Line 23:</td> <td colspan="2" class="diff-lineno">Line 23:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  <del style="font-weight: bold; text-decoration: none;">[</del>https://<del style="font-weight: bold; text-decoration: none;">pubs</del>.<del style="font-weight: bold; text-decoration: none;">er</del>.<del style="font-weight: bold; text-decoration: none;">usgs.gov/publication</del>/sir20175009/ upper Colorado River Basin salinity]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  https://<ins style="font-weight: bold; text-decoration: none;">doi</ins>.<ins style="font-weight: bold; text-decoration: none;">org/10</ins>.<ins style="font-weight: bold; text-decoration: none;">3133</ins>/sir20175009/ upper Colorado River Basin salinity]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=3106&oldid=prev 2022-11-29T15:12:35Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:12, 29 November 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l23">Line 23:</td> <td colspan="2" class="diff-lineno">Line 23:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  [https://pubs.usgs.gov/<del style="font-weight: bold; text-decoration: none;">sir/2017/5009</del>/sir20175009<del style="font-weight: bold; text-decoration: none;">.pdf</del>/ upper Colorado River Basin salinity]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://doi.org/10.3133/sir20175009] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  [https://pubs<ins style="font-weight: bold; text-decoration: none;">.er</ins>.usgs.gov/<ins style="font-weight: bold; text-decoration: none;">publication</ins>/sir20175009/ upper Colorado River Basin salinity]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=3105&oldid=prev 2022-11-29T15:11:14Z

<p></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 11:11, 29 November 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l23">Line 23:</td> <td colspan="2" class="diff-lineno">Line 23:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Both historical and future salinity and salt loads have been estimated using a variety of models. NRCS USGS, and Reclamation have used the SLOAD, and SPARROW models to estimate salinity in the Colorado River.</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">[https://pubs.er.usgs.gov/publication/wri864124/ SLOAD] (Salinity LOAD) - USGS </del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://<ins style="font-weight: bold; text-decoration: none;">doi</ins>.<ins style="font-weight: bold; text-decoration: none;">org/10</ins>.<ins style="font-weight: bold; text-decoration: none;">3133</ins>/<ins style="font-weight: bold; text-decoration: none;">sir20175009</ins>] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  [https://pubs.usgs.gov/sir/2017/5009/sir20175009.pdf/ upper Colorado River Basin salinity]</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>SPARROW  (SPAtially Referenced Regression On Watershed attributes) - USGS [https://<del style="font-weight: bold; text-decoration: none;">pubs</del>.<del style="font-weight: bold; text-decoration: none;">usgs</del>.<del style="font-weight: bold; text-decoration: none;">gov</del>/<del style="font-weight: bold; text-decoration: none;">tm/2006/tm6b3/contents.htm</del>] SPARROW uses nonlinear regression equations to estimate the  transport of analytes (such as salts) through river networks, including estimates of  [https://pubs.usgs.gov/sir/2017/5009/sir20175009.pdf/ upper Colorado River Basin salinity]</div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>&lt;/onlyinclude&gt;</div></td></tr> </table>

TanyaPetach http://coloradoriverscience.org/index.php?title=Salinity&diff=2809&oldid=prev 2022-09-13T17:54:00Z

<p><span class="autocomment">Data and Tools</span></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:54, 13 September 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l14">Line 14:</td> <td colspan="2" class="diff-lineno">Line 14:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Data and Tools==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Data and Tools==</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div> </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">&lt;onlyinclude&gt;</ins></div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Observed Salinity===</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>===Observed Salinity===</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;">&lt;onlyinclude&gt;</del></div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity Control Monitoring Reports  </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity Control Monitoring Reports  </div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> </table>

JeffreyJLukas http://coloradoriverscience.org/index.php?title=Salinity&diff=2807&oldid=prev 2022-09-13T17:49:28Z

<p><span class="autocomment">Overview</span></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:49, 13 September 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l4">Line 4:</td> <td colspan="2" class="diff-lineno">Line 4:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Following protests in Mexico about the excessive salinity of the Colorado River water deliveries to Mexico and implicit violations of the 1944 US-Mexico Water Treaty, salinity control measures were established across the Colorado River Basin. The Colorado River Basin Salinity Control Act (1973) established salinity criteria at three monitoring locations along the River and required the implementation of salinity control programs. The monitoring locations and target salinity concentrations are: below Hoover Dam (723 mg/L), below Parker Dam (747 mg/L), and at Imperial Dam (879 mg/L).</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Following protests in Mexico about the excessive salinity of the Colorado River water deliveries to Mexico and implicit violations of the 1944 US-Mexico Water Treaty, salinity control measures were established across the Colorado River Basin. The Colorado River Basin Salinity Control Act (1973) established salinity criteria at three monitoring locations along the River and required the implementation of salinity control programs. The monitoring locations and target salinity concentrations are: below Hoover Dam (723 mg/L), below Parker Dam (747 mg/L), and at Imperial Dam (879 mg/L).</div></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div><del style="font-weight: bold; text-decoration: none;"></del></div></td><td colspan="2" class="diff-side-added"></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The salinity control programs include salinity control units at Paradox Valley (CO), Grand Valley (CO), Las Vegas Wash (NV), and Crystal Geyser (UT) in addition to voluntary on-farm salinity control programs. Salinity control measures were estimated to control 1.22 million tons of salt annually in 2020 (about 10-12% of the salinity measured below Hoover Dam). Minute No. 242 mandates that the salinity of water deliveries to Mexico upstream of the Morelos Dam be no more than 115 ± 30 mg/L above average annual flow-weighted salinity of the Colorado River arriving at Imperial Dam.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The salinity control programs include salinity control units at Paradox Valley (CO), Grand Valley (CO), Las Vegas Wash (NV), and Crystal Geyser (UT) in addition to voluntary on-farm salinity control programs. Salinity control measures were estimated to control 1.22 million tons of salt annually in 2020 (about 10-12% of the salinity measured below Hoover Dam). Minute No. 242 mandates that the salinity of water deliveries to Mexico upstream of the Morelos Dam be no more than 115 ± 30 mg/L above average annual flow-weighted salinity of the Colorado River arriving at Imperial Dam.</div></td></tr> </table>

JeffreyJLukas http://coloradoriverscience.org/index.php?title=Salinity&diff=2806&oldid=prev 2022-09-13T17:49:12Z

<p><span class="autocomment">Overview</span></p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 13:49, 13 September 2022</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Overview==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Overview==</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>[[File:Salinity_Figure2.png|thumb|<del style="font-weight: bold; text-decoration: none;">550px</del>|'''Figure 1.''' Flow and salinity in the Colorado River Basin, showing how salinity (salt concentration) increases downstream from the headwaters, especially below Glen Canyon Dam.  (Bureau of Reclamation)]]</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>[[File:Salinity_Figure2.png|thumb|<ins style="font-weight: bold; text-decoration: none;">500px</ins>|'''Figure 1.''' Flow and salinity in the Colorado River Basin, showing how salinity (salt concentration) increases downstream from the headwaters, especially below Glen Canyon Dam.  (Bureau of Reclamation)]]</div></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr> <tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Salinity refers to the concentration of dissolved salts–most commonly sodium chloride (table salt NaCl) but also magnesium sulfate, potassium nitrate, and sodium bicarbonate. Salinity in the Colorado River increases as it flows downstream (Figure 1) due to accumulation and concentration of salts from both natural and man-made sources and causes. Natural sources (e.g. saline springs, concentration due to evaporation and transpiration, erosion and dissolution of sediments, etc.)  account for approximately half of the salinity as measured at Hoover Dam. The remaining half of the salinity contributions are due to human activities and are split between out of basin exports (3%), agricultural irrigation (37%), reservoir evaporation and plant consumption (12%), and municipal and industrial uses (1%). In total, approximately 9 million tons of salts flow past the Hoover Dam annually.</div></td></tr> </table>

JeffreyJLukas