https://jams.uni-jena.de/ilmswiki/index.php?action=history&feed=atom&title=Soil_parameterizationSoil parameterization - Revision history2026-05-31T09:21:08ZRevision history for this page on the wikiMediaWiki 1.17.0https://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=12954&oldid=prevDanielS at 13:40, 10 March 20132013-03-10T13:40:56Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Note down the value in the volume Qr which is 'Residual Water Content' equivalent to wilting point. The value represents the water content in 15,000 mbar pressure.</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Note down the value in the volume Qr which is 'Residual Water Content' equivalent to wilting point. The value represents the water content in 15,000 mbar pressure.</div></td></tr>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>Click ‘Next’ a new <del class="diffchange diffchange-inline">windows appear</del>.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>Click ‘Next’<ins class="diffchange diffchange-inline">, </ins>a new <ins class="diffchange diffchange-inline">window will come up</ins>.</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:waterflowboundary.png|soilType-A]]</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:waterflowboundary.png|soilType-A]]</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=12953&oldid=prevDanielS at 13:01, 10 March 20132013-03-10T13:01:49Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:Newproject_soiltypeA.png|soilType-A]]</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:Newproject_soiltypeA.png|soilType-A]]</div></td></tr>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>On pre-processing <del class="diffchange diffchange-inline">windows </del>select the “Water Flow – Soil Hydraulic Parameters”</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>On <ins class="diffchange diffchange-inline">the </ins>pre-processing <ins class="diffchange diffchange-inline">window </ins>select the “Water Flow – Soil Hydraulic Parameters”</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The new window will appear:</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>The new window will appear:</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=12952&oldid=prevDanielS at 12:36, 10 March 20132013-03-10T12:36:38Z<p></p>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The texture information needs to be supplied to HYDRUS-1D software to <del class="diffchange diffchange-inline">get </del>the water holding capacity of the specific texture combination:</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The texture information needs to be supplied to <ins class="diffchange diffchange-inline">the </ins>HYDRUS-1D software to <ins class="diffchange diffchange-inline">obtain </ins>the water holding capacity of the specific texture combination:</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>*The HYDRUS-1D can be download from the following link: http://www.pc-progress.com/en/Default.aspx?hydrus-1d</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>*The HYDRUS-1D can be download from the following link: http://www.pc-progress.com/en/Default.aspx?hydrus-1d</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=12951&oldid=prevDanielS at 12:22, 10 March 20132013-03-10T12:22:09Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[pt:Parametrização_do_solo]]</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[pt:Parametrização_do_solo]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>To develop the soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage <del class="diffchange diffchange-inline">are </del>required. This information is general available in the soil dataset. The texture information is useful to describe the characteristics of the soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios, namely: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of the soil (Scheffer and Schachtschabel 1984).  </div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>To develop the soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage <ins class="diffchange diffchange-inline">is </ins>required. This information is general available in the soil dataset. The texture information is useful to describe the characteristics of the soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios, namely: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of the soil (Scheffer and Schachtschabel 1984).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=12950&oldid=prevDanielS at 12:21, 10 March 20132013-03-10T12:21:04Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[pt:Parametrização_do_solo]]</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[pt:Parametrização_do_solo]]</div></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage <del class="diffchange diffchange-inline">is </del>required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios<del class="diffchange diffchange-inline">. They are</del>: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>To develop <ins class="diffchange diffchange-inline">the </ins>soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage <ins class="diffchange diffchange-inline">are </ins>required. This information is general available in <ins class="diffchange diffchange-inline">the </ins>soil dataset. The texture information is useful to describe the characteristics of <ins class="diffchange diffchange-inline">the </ins>soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios<ins class="diffchange diffchange-inline">, namely</ins>: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of <ins class="diffchange diffchange-inline">the </ins>soil (Scheffer and Schachtschabel 1984).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=11805&oldid=prevDanielS at 13:09, 3 October 20122012-10-03T13:09:42Z<p></p>
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<tr><td colspan="2"> </td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div><ins style="color: red; font-weight: bold; text-decoration: none;">[[pt:Parametrização_do_solo]]</ins></div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS-1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
</table>DanielShttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=11731&oldid=prevSantosh at 08:15, 1 October 20122012-10-01T08:15:35Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Select model of “% Sand, Silt and Clay (SSC)”.  </div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>Select model of “% Sand, Silt and Clay (SSC)”.  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>Input the percentage of SSC in the window. In this example, the SSC of A-horizon from the table above is provided.</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>Input the percentage of SSC in the window. In this example, the SSC of A-horizon from the table above is provided<ins class="diffchange diffchange-inline">. In case the information is not available, users can put the qualitative information about the soil class under 'Textural class' of Input section</ins>.</div></td></tr>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:texture_input2.png|soilType-A]]</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>[[File:texture_input2.png|soilType-A]]</div></td></tr>
</table>Santoshhttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=11730&oldid=prevSantosh at 08:06, 1 October 20122012-10-01T08:06:05Z<p></p>
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<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>|}</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>|}</div></td></tr>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>The texture information needs to be supplied to HYDRUS 1D software to get the water holding capacity of the specific texture combination:</div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>The texture information needs to be supplied to HYDRUS<ins class="diffchange diffchange-inline">-</ins>1D software to get the water holding capacity of the specific texture combination:</div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>*The HYDRUS-1D can be download from the following link: http://www.pc-progress.com/en/Default.aspx?hydrus-1d</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>*The HYDRUS-1D can be download from the following link: http://www.pc-progress.com/en/Default.aspx?hydrus-1d</div></td></tr>
</table>Santoshhttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=11729&oldid=prevSantosh at 08:02, 1 October 20122012-10-01T08:02:10Z<p></p>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS 1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component Rosetta inside 'HYDRUS<ins class="diffchange diffchange-inline">-</ins>1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td></tr>
</table>Santoshhttps://jams.uni-jena.de/ilmswiki/index.php?title=Soil_parameterization&diff=11728&oldid=prevSantosh at 08:01, 1 October 20122012-10-01T08:01:52Z<p></p>
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<tr><td class='diff-marker'>−</td><td style="background: #ffa; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component <del class="diffchange diffchange-inline">ROsetta </del>inside 'HYDRUS 1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984). <del class="diffchange diffchange-inline">The soil texture information provides additional</del></div></td><td class='diff-marker'>+</td><td style="background: #cfc; color:black; font-size: smaller;"><div>To develop soil parameterization file, first the depth of the different soil horizons and texture (combination of soil, silt and clay) in percentage is required. This information is general available in soil dataset. The texture information is useful to describe the characteristics of soil water retention curve. The soil texture information (in percentage) is  provided as input data to the software component <ins class="diffchange diffchange-inline">Rosetta </ins>inside 'HYDRUS 1D' to understand pedotransfer functions of soils in three different hypothetical pressure scenarios. They are: 0 mbar, 60 mbar and 15,000 mbar. The soil texture is classified according to the specific pore volumes of soil (Scheffer and Schachtschabel 1984).  </div></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"></td></tr>
<tr><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td><td class='diff-marker'> </td><td style="background: #eee; color:black; font-size: smaller;"><div>For example, a soil type A has following depth and texture combination:</div></td></tr>
</table>Santosh