https://damtoolbox.org/index.php?action=history&feed=atom&title=GroundwaterGroundwater - Revision history2026-04-11T16:40:14ZRevision history for this page on the wikiMediaWiki 1.40.0https://damtoolbox.org/index.php?title=Groundwater&diff=7372&oldid=prevMpollei@gfnet.com at 05:05, 21 July 20232023-07-21T05:05:51Z<p></p>
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<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>==Best Practices Resources==</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>==Best Practices Resources==</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>{{Document Icon}} [[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology, NRCS<del style="font-weight: bold; text-decoration: none;">, 2010</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>{{Document Icon}} [[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology, NRCS]]</div></td></tr>
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<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><!-- In the location of an in text citation, simply enclose the citation as follows: <ref> citation </ref>. Citations will automatically populate. Learn more at https://www.mediawiki.org/wiki/Help:Cite. --></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><!-- In the location of an in text citation, simply enclose the citation as follows: <ref> citation </ref>. Citations will automatically populate. Learn more at https://www.mediawiki.org/wiki/Help:Cite. --></div></td></tr>
</table>Mpollei@gfnet.comhttps://damtoolbox.org/index.php?title=Groundwater&diff=6670&oldid=prevGrichards at 22:14, 16 March 20232023-03-16T22:14:56Z<p></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:14, 16 March 2023</td>
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<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>"Water exists in the atmosphere, on the Earth’s surface (the hydrosphere), and under the Earth’s surface (the lithosphere). A continual interchange produces a closed system that is known as the hydrologic cycle. Water in the lithosphere is in the form of free water, water vapor, or ice, or is chemically combined with earth materials. Uncombined water occupies the void spaces. The interstices may be occupied by air or other gases or by water or other liquids. A rock or soil is said to be porous or to have porosity if it contains interstices or voids. Porosity can be quantitatively expressed as the ratio of the total volume of voids to the total volume of the rock or soil. It is usually given as a percentage. Primary porosity is a result of the processes that formed rock or soil. Secondary porosity is produced by fracture, solution, or recrystallization. Groundwater occurs in both primary and secondary voids."<ref name="NEH">[[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology, NRCS, 2010]]</ref> </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>"Water exists in the atmosphere, on the Earth’s surface (the hydrosphere), and under the Earth’s surface (the lithosphere). A continual interchange produces a closed system that is known as the hydrologic cycle. Water in the lithosphere is in the form of free water, water vapor, or ice, or is chemically combined with earth materials. Uncombined water occupies the void spaces. The interstices may be occupied by air or other gases or by water or other liquids. A rock or soil is said to be porous or to have porosity if it contains interstices or voids. Porosity can be quantitatively expressed as the ratio of the total volume of voids to the total volume of the rock or soil. It is usually given as a percentage. Primary porosity is a result of the processes that formed rock or soil. Secondary porosity is produced by fracture, solution, or recrystallization. Groundwater occurs in both primary and secondary voids."<ref name="NEH">[[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology, NRCS, 2010]]</ref> </div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></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;"></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></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;">Groundwater is not typically considered in hydrologic analysis of dams other than the conservative assumption that the basin [[soils]] are saturated prior to the [[precipitation]] event. However, some states are recognizing the influence of groundwater on runoff, particularly for basins with well-drained, but thin soil profiles where saturation excess runoff (i.e., interflow) becomes important in driving runoff during the peak of the hydrograph. This differs from the more traditional assumption of infiltration excess runoff where the soil profile is considered an infinite sink. </ins></div></td></tr>
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</table>Grichardshttps://damtoolbox.org/index.php?title=Groundwater&diff=6013&oldid=prevRmanwaring at 20:29, 19 December 20222022-12-19T20:29:29Z<p></p>
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<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>----</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>----</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>"Water exists in the atmosphere, on the Earth’s surface (the hydrosphere), and under the Earth’s surface (the lithosphere). A continual interchange produces a closed system that is known as the hydrologic cycle. Water in the lithosphere is in the form of free water, water vapor, or ice, or is chemically combined with earth materials. Uncombined water occupies the void spaces. The interstices may be occupied by air or other gases or by water or other liquids. A rock or soil is said to be porous or to have porosity if it contains interstices or voids. Porosity can be quantitatively expressed as the ratio of the total volume of voids to the total volume of the rock or soil. It is usually given as a percentage. Primary porosity is a result of the processes that formed rock or soil. Secondary porosity is produced by fracture, solution, or recrystallization. Groundwater occurs in both primary and secondary voids."<ref name="NEH">[[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology|National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology <del style="font-weight: bold; text-decoration: none;">(</del>NRCS, 2010<del style="font-weight: bold; text-decoration: none;">)</del>]]</ref> </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>"Water exists in the atmosphere, on the Earth’s surface (the hydrosphere), and under the Earth’s surface (the lithosphere). A continual interchange produces a closed system that is known as the hydrologic cycle. Water in the lithosphere is in the form of free water, water vapor, or ice, or is chemically combined with earth materials. Uncombined water occupies the void spaces. The interstices may be occupied by air or other gases or by water or other liquids. A rock or soil is said to be porous or to have porosity if it contains interstices or voids. Porosity can be quantitatively expressed as the ratio of the total volume of voids to the total volume of the rock or soil. It is usually given as a percentage. Primary porosity is a result of the processes that formed rock or soil. Secondary porosity is produced by fracture, solution, or recrystallization. Groundwater occurs in both primary and secondary voids."<ref name="NEH">[[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology<ins style="font-weight: bold; text-decoration: none;">, </ins>NRCS, 2010]]</ref> </div></td></tr>
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<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>==Best Practices Resources==</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>==Best Practices Resources==</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>{{Document Icon}} [[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology <del style="font-weight: bold; text-decoration: none;">(Natural Resources Conservation Service)</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>{{Document Icon}} [[National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology | National Engineering Handbook: Chapter 30 - Groundwater Hydrology and Geology<ins style="font-weight: bold; text-decoration: none;">, NRCS, 2010</ins>]]</div></td></tr>
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<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><!-- In the location of an in text citation, simply enclose the citation as follows: <ref> citation </ref>. Citations will automatically populate. Learn more at https://www.mediawiki.org/wiki/Help:Cite. --></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><!-- In the location of an in text citation, simply enclose the citation as follows: <ref> citation </ref>. Citations will automatically populate. Learn more at https://www.mediawiki.org/wiki/Help:Cite. --></div></td></tr>
</table>Rmanwaringhttps://damtoolbox.org/index.php?title=Groundwater&diff=5243&oldid=prevGrichards at 04:34, 13 December 20222022-12-13T04:34:41Z<p></p>
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<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;">!-- Introductory paragraph or topic page summary </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;">"Water exists in the atmosphere, on the Earth’s surface (the hydrosphere), and under the Earth’s surface (the lithosphere). A continual interchange produces a closed system that is known as the hydrologic cycle. Water in the lithosphere is in the form of free water, water vapor, or ice, or is chemically combined with earth materials. Uncombined water occupies the void spaces. The interstices may be occupied by air or other gases or by water or other liquids. A rock or soil is said to be porous or to have porosity if it contains interstices or voids. Porosity can be quantitatively expressed as the ratio of the total volume of voids to the total volume of the rock or soil. It is usually given as a percentage. Primary porosity is a result of the processes that formed rock or soil. Secondary porosity is produced by fracture, solution, or recrystallization. Groundwater occurs in both primary and secondary voids."</ins><<ins style="font-weight: bold; text-decoration: none;">ref name="NEH">[[National Engineering Handbook: Chapter 30 </ins>- <ins style="font-weight: bold; text-decoration: none;">Groundwater Hydrology and Geology|National Engineering Handbook: Chapter 30 </ins>- <ins style="font-weight: bold; text-decoration: none;">Groundwater Hydrology and Geology (NRCS, 2010)]]</ref</ins>> </div></td></tr>
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</table>Grichardshttps://damtoolbox.org/index.php?title=Groundwater&diff=4280&oldid=prevGrichards at 02:16, 18 November 20222022-11-18T02:16:01Z<p></p>
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</table>Grichardshttps://damtoolbox.org/index.php?title=Groundwater&diff=3995&oldid=prevRmanwaring at 19:41, 21 October 20222022-10-21T19:41:55Z<p></p>
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</table>Rmanwaringhttps://damtoolbox.org/index.php?title=Groundwater&diff=3670&oldid=prevGrichards: Created page with "<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed --> __NOTOC__ ---- <!-- Introductory paragraph or topic page summary --> Paragraph text ==Best Practices Resources== {{Document Icon}} National Engineering Handbook: Chapter 30- Groundwater Hydrology and Geology (Natural Resources Conservation Service) <!-- In the location of an in text..."2022-09-17T03:11:28Z<p>Created page with "<!-- Delete any sections that are not necessary to your topic. Add pictures/sections as needed --> __NOTOC__ ---- <!-- Introductory paragraph or topic page summary --> Paragraph text ==Best Practices Resources== {{Document Icon}} <a href="/wiki/Geology_National_Engineering_Handbook:_Chapter_30-_Groundwater_Hydrology_and_Geology" title="Geology National Engineering Handbook: Chapter 30- Groundwater Hydrology and Geology"> National Engineering Handbook: Chapter 30- Groundwater Hydrology and Geology (Natural Resources Conservation Service)</a> <!-- In the location of an in text..."</p>
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