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New Conceptual Model for Soil Treatment Units: Formation of Multiple Hydraulic Zones during Unsaturated Wastewater Infiltration
Onsite wastewater treatment systems are commonly used in the United States to reclaim domestic wastewater. A distinct biomat forms at the infiltrative surface, causing resistance to flow and decreasing soil moisture below the biomat. To simulate these conditions, previous modeling studies have used...
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Published in: | Journal of environmental quality 2013-07, Vol.42 (4), p.1196-1204 |
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description | Onsite wastewater treatment systems are commonly used in the United States to reclaim domestic wastewater. A distinct biomat forms at the infiltrative surface, causing resistance to flow and decreasing soil moisture below the biomat. To simulate these conditions, previous modeling studies have used a two‐layer approach: a thin biomat layer (1–5 cm thick) and the native soil layer below the biomat. However, the effect of wastewater application extends below the biomat layer. We used numerical modeling supported by experimental data to justify a new conceptual model that includes an intermediate zone (IZ) below the biomat. The conceptual model was set up using Hydrus 2D and calibrated against soil moisture and water flux measurements. The estimated hydraulic conductivity value for the IZ was between biomat and the native soil. The IZ has important implications for wastewater treatment. When the IZ was not considered, a loading rate of 5 cm d−1 resulted in an 8.5‐cm ponding. With the IZ, the same loading rate resulted in a 9.5‐cm ponding. Without the IZ, up to 3.1 cm d−1 of wastewater could be applied without ponding; with the IZ, only up to 2.8 cm d−1 could be applied without ponding. The IZ also plays a significant role in soil moisture distribution. Without the IZ, near‐saturation conditions were observed only within the biomat, whereas near‐saturation conditions extended below the biomat with the IZ. Accurate prediction of ponding is important to prevent surfacing of wastewater. The degree of water and air saturation influences pollutant treatment efficiency through residence time, volatility, and biochemical reactions. |
doi_str_mv | 10.2134/jeq2012.0441 |
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A distinct biomat forms at the infiltrative surface, causing resistance to flow and decreasing soil moisture below the biomat. To simulate these conditions, previous modeling studies have used a two‐layer approach: a thin biomat layer (1–5 cm thick) and the native soil layer below the biomat. However, the effect of wastewater application extends below the biomat layer. We used numerical modeling supported by experimental data to justify a new conceptual model that includes an intermediate zone (IZ) below the biomat. The conceptual model was set up using Hydrus 2D and calibrated against soil moisture and water flux measurements. The estimated hydraulic conductivity value for the IZ was between biomat and the native soil. The IZ has important implications for wastewater treatment. When the IZ was not considered, a loading rate of 5 cm d−1 resulted in an 8.5‐cm ponding. With the IZ, the same loading rate resulted in a 9.5‐cm ponding. Without the IZ, up to 3.1 cm d−1 of wastewater could be applied without ponding; with the IZ, only up to 2.8 cm d−1 could be applied without ponding. The IZ also plays a significant role in soil moisture distribution. Without the IZ, near‐saturation conditions were observed only within the biomat, whereas near‐saturation conditions extended below the biomat with the IZ. Accurate prediction of ponding is important to prevent surfacing of wastewater. The degree of water and air saturation influences pollutant treatment efficiency through residence time, volatility, and biochemical reactions.</description><identifier>ISSN: 0047-2425</identifier><identifier>EISSN: 1537-2537</identifier><identifier>DOI: 10.2134/jeq2012.0441</identifier><identifier>PMID: 24216371</identifier><identifier>CODEN: JEVQAA</identifier><language>eng</language><publisher>United States: The American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc</publisher><subject>Conductivity ; Domestic wastewater ; Effluents ; Flow resistance ; Fluid flow ; Hydraulics ; Influence ; Load distribution ; Mathematical models ; Microorganisms ; Moisture content ; Organic chemicals ; Ponding ; Saturation ; Sensitivity analysis ; Soil ; Soil (material) ; Soil moisture ; Soil treatment ; Viruses ; Waste Disposal, Fluid ; Waste Water ; Wastewater treatment ; Water Movements ; Water Purification</subject><ispartof>Journal of environmental quality, 2013-07, Vol.42 (4), p.1196-1204</ispartof><rights>Copyright © by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc.</rights><rights>Copyright American Society of Agronomy Jul/Aug 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4351-e624e7abc2e1b6f05e628ca70f31f56affa44437320188bc5ddc816ba57a63de3</citedby><cites>FETCH-LOGICAL-c4351-e624e7abc2e1b6f05e628ca70f31f56affa44437320188bc5ddc816ba57a63de3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/24216371$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Geza, Mengistu</creatorcontrib><creatorcontrib>Lowe, Kathryn S.</creatorcontrib><creatorcontrib>Huntzinger, Deborah N.</creatorcontrib><creatorcontrib>McCray, John E.</creatorcontrib><title>New Conceptual Model for Soil Treatment Units: Formation of Multiple Hydraulic Zones during Unsaturated Wastewater Infiltration</title><title>Journal of environmental quality</title><addtitle>J Environ Qual</addtitle><description>Onsite wastewater treatment systems are commonly used in the United States to reclaim domestic wastewater. A distinct biomat forms at the infiltrative surface, causing resistance to flow and decreasing soil moisture below the biomat. To simulate these conditions, previous modeling studies have used a two‐layer approach: a thin biomat layer (1–5 cm thick) and the native soil layer below the biomat. However, the effect of wastewater application extends below the biomat layer. We used numerical modeling supported by experimental data to justify a new conceptual model that includes an intermediate zone (IZ) below the biomat. The conceptual model was set up using Hydrus 2D and calibrated against soil moisture and water flux measurements. The estimated hydraulic conductivity value for the IZ was between biomat and the native soil. The IZ has important implications for wastewater treatment. When the IZ was not considered, a loading rate of 5 cm d−1 resulted in an 8.5‐cm ponding. With the IZ, the same loading rate resulted in a 9.5‐cm ponding. Without the IZ, up to 3.1 cm d−1 of wastewater could be applied without ponding; with the IZ, only up to 2.8 cm d−1 could be applied without ponding. The IZ also plays a significant role in soil moisture distribution. Without the IZ, near‐saturation conditions were observed only within the biomat, whereas near‐saturation conditions extended below the biomat with the IZ. Accurate prediction of ponding is important to prevent surfacing of wastewater. The degree of water and air saturation influences pollutant treatment efficiency through residence time, volatility, and biochemical reactions.</description><subject>Conductivity</subject><subject>Domestic wastewater</subject><subject>Effluents</subject><subject>Flow resistance</subject><subject>Fluid flow</subject><subject>Hydraulics</subject><subject>Influence</subject><subject>Load distribution</subject><subject>Mathematical models</subject><subject>Microorganisms</subject><subject>Moisture content</subject><subject>Organic chemicals</subject><subject>Ponding</subject><subject>Saturation</subject><subject>Sensitivity analysis</subject><subject>Soil</subject><subject>Soil (material)</subject><subject>Soil moisture</subject><subject>Soil treatment</subject><subject>Viruses</subject><subject>Waste Disposal, Fluid</subject><subject>Waste Water</subject><subject>Wastewater treatment</subject><subject>Water Movements</subject><subject>Water 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E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>New Conceptual Model for Soil Treatment Units: Formation of Multiple Hydraulic Zones during Unsaturated Wastewater Infiltration</atitle><jtitle>Journal of environmental quality</jtitle><addtitle>J Environ Qual</addtitle><date>2013-07</date><risdate>2013</risdate><volume>42</volume><issue>4</issue><spage>1196</spage><epage>1204</epage><pages>1196-1204</pages><issn>0047-2425</issn><eissn>1537-2537</eissn><coden>JEVQAA</coden><abstract>Onsite wastewater treatment systems are commonly used in the United States to reclaim domestic wastewater. A distinct biomat forms at the infiltrative surface, causing resistance to flow and decreasing soil moisture below the biomat. To simulate these conditions, previous modeling studies have used a two‐layer approach: a thin biomat layer (1–5 cm thick) and the native soil layer below the biomat. However, the effect of wastewater application extends below the biomat layer. We used numerical modeling supported by experimental data to justify a new conceptual model that includes an intermediate zone (IZ) below the biomat. The conceptual model was set up using Hydrus 2D and calibrated against soil moisture and water flux measurements. The estimated hydraulic conductivity value for the IZ was between biomat and the native soil. The IZ has important implications for wastewater treatment. When the IZ was not considered, a loading rate of 5 cm d−1 resulted in an 8.5‐cm ponding. With the IZ, the same loading rate resulted in a 9.5‐cm ponding. Without the IZ, up to 3.1 cm d−1 of wastewater could be applied without ponding; with the IZ, only up to 2.8 cm d−1 could be applied without ponding. The IZ also plays a significant role in soil moisture distribution. Without the IZ, near‐saturation conditions were observed only within the biomat, whereas near‐saturation conditions extended below the biomat with the IZ. Accurate prediction of ponding is important to prevent surfacing of wastewater. The degree of water and air saturation influences pollutant treatment efficiency through residence time, volatility, and biochemical reactions.</abstract><cop>United States</cop><pub>The American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, Inc</pub><pmid>24216371</pmid><doi>10.2134/jeq2012.0441</doi><tpages>9</tpages></addata></record> |
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subjects | Conductivity Domestic wastewater Effluents Flow resistance Fluid flow Hydraulics Influence Load distribution Mathematical models Microorganisms Moisture content Organic chemicals Ponding Saturation Sensitivity analysis Soil Soil (material) Soil moisture Soil treatment Viruses Waste Disposal, Fluid Waste Water Wastewater treatment Water Movements Water Purification |
title | New Conceptual Model for Soil Treatment Units: Formation of Multiple Hydraulic Zones during Unsaturated Wastewater Infiltration |
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