Effect of water table level on CO2, CH4 and N2O emissions in a freshwater marsh of Northeast China

We quantified the effects of the water table on CO2, CH4 and N2O emissions from microcosms in a freshwater marsh in Sanjiang Plain, Northeast China. From July to September in 2005, CO2, CH4 and N2O emission rates were measured in an undisturbed natural marsh (in natural) and microcosms of three mani...

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Veröffentlicht in:Soil biology & biochemistry 2013-06, Vol.61, p.52-60
Hauptverfasser: Yang, Jisong, Liu, Jingshuang, Hu, Xiaojun, Li, Xinxin, Wang, Yan, Li, Huiying
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container_start_page 52
container_title Soil biology & biochemistry
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creator Yang, Jisong
Liu, Jingshuang
Hu, Xiaojun
Li, Xinxin
Wang, Yan
Li, Huiying
description We quantified the effects of the water table on CO2, CH4 and N2O emissions from microcosms in a freshwater marsh in Sanjiang Plain, Northeast China. From July to September in 2005, CO2, CH4 and N2O emission rates were measured in an undisturbed natural marsh (in natural) and microcosms of three manipulated water table treatments: a reference, a high water table (HW) and a low water table (LW). The averages of CO2, CH4 and N2O emissions were 360.2 mg m−2 h−1, 7.43 mg m−2 h−1 and 12.84 μg m−2 h−1, respectively, close to those in reference (p 
doi_str_mv 10.1016/j.soilbio.2013.02.009
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From July to September in 2005, CO2, CH4 and N2O emission rates were measured in an undisturbed natural marsh (in natural) and microcosms of three manipulated water table treatments: a reference, a high water table (HW) and a low water table (LW). The averages of CO2, CH4 and N2O emissions were 360.2 mg m−2 h−1, 7.43 mg m−2 h−1 and 12.84 μg m−2 h−1, respectively, close to those in reference (p &lt; 0.05), averaging 394.5 mg m−2 h−1, 8.92 mg m−2 h−1 and 13.3 μg m−2 h−1. This means microcosm installation had no significant effect on CO2 efflux. Averaged CO2 (p = 0.03) and CH4 (p = 0.001) emissions were significantly different across the treatments, but that of N2O emission (p = 0.36) was not. To quantify the effects of water table position, three typical classes of water table were considered, i.e. +2 to +14 cm, –11 to 0 cm and −28 to −11.3 cm (+, above the soil surface. –, below the soil surface). Mean CO2 and N2O emissions were lowest at the higher water table positions (+2 to +14 cm) and increased by 120% and 60% at the lower water table positions (−11 to 0 cm), respectively, and the corresponding CH4 emissions decreased by 75%. However, at lowest water table positions (−28 to −11.3 cm), little additional effects on gas emissions were not found. Our results suggested that there could be considerable changes of greenhouse emissions as a response of water drawdown due to wetland drainage. ► Three manipulating water table levels were successfully conducted in a marsh. ► Gas emissions had differences at different water table positions. ► CO2 and N2O emissions were higher when water table below the soil surface. ► CH4 emission were higher when water table above the soil surface. ► There were considerable changes of gas emissions as a response of water drawdown.</description><identifier>ISSN: 0038-0717</identifier><identifier>EISSN: 1879-3428</identifier><identifier>DOI: 10.1016/j.soilbio.2013.02.009</identifier><identifier>CODEN: SBIOAH</identifier><language>eng</language><publisher>Amsterdam: Elsevier Ltd</publisher><subject>Agronomy. 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From July to September in 2005, CO2, CH4 and N2O emission rates were measured in an undisturbed natural marsh (in natural) and microcosms of three manipulated water table treatments: a reference, a high water table (HW) and a low water table (LW). The averages of CO2, CH4 and N2O emissions were 360.2 mg m−2 h−1, 7.43 mg m−2 h−1 and 12.84 μg m−2 h−1, respectively, close to those in reference (p &lt; 0.05), averaging 394.5 mg m−2 h−1, 8.92 mg m−2 h−1 and 13.3 μg m−2 h−1. This means microcosm installation had no significant effect on CO2 efflux. Averaged CO2 (p = 0.03) and CH4 (p = 0.001) emissions were significantly different across the treatments, but that of N2O emission (p = 0.36) was not. To quantify the effects of water table position, three typical classes of water table were considered, i.e. +2 to +14 cm, –11 to 0 cm and −28 to −11.3 cm (+, above the soil surface. –, below the soil surface). Mean CO2 and N2O emissions were lowest at the higher water table positions (+2 to +14 cm) and increased by 120% and 60% at the lower water table positions (−11 to 0 cm), respectively, and the corresponding CH4 emissions decreased by 75%. However, at lowest water table positions (−28 to −11.3 cm), little additional effects on gas emissions were not found. Our results suggested that there could be considerable changes of greenhouse emissions as a response of water drawdown due to wetland drainage. ► Three manipulating water table levels were successfully conducted in a marsh. ► Gas emissions had differences at different water table positions. ► CO2 and N2O emissions were higher when water table below the soil surface. ► CH4 emission were higher when water table above the soil surface. ► There were considerable changes of gas emissions as a response of water drawdown.</description><subject>Agronomy. 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Psychology</topic><topic>gas emissions</topic><topic>greenhouse gases</topic><topic>high water table</topic><topic>Marsh</topic><topic>marshes</topic><topic>Methane</topic><topic>Microcosm</topic><topic>Nitrous oxide</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>soil</topic><topic>Soil science</topic><topic>Water table</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Jisong</creatorcontrib><creatorcontrib>Liu, Jingshuang</creatorcontrib><creatorcontrib>Hu, Xiaojun</creatorcontrib><creatorcontrib>Li, Xinxin</creatorcontrib><creatorcontrib>Wang, Yan</creatorcontrib><creatorcontrib>Li, Huiying</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 1: Biological Sciences &amp; Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 3: Aquatic Pollution &amp; Environmental Quality</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Soil biology &amp; biochemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yang, Jisong</au><au>Liu, Jingshuang</au><au>Hu, Xiaojun</au><au>Li, Xinxin</au><au>Wang, Yan</au><au>Li, Huiying</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Effect of water table level on CO2, CH4 and N2O emissions in a freshwater marsh of Northeast China</atitle><jtitle>Soil biology &amp; biochemistry</jtitle><date>2013-06-01</date><risdate>2013</risdate><volume>61</volume><spage>52</spage><epage>60</epage><pages>52-60</pages><issn>0038-0717</issn><eissn>1879-3428</eissn><coden>SBIOAH</coden><abstract>We quantified the effects of the water table on CO2, CH4 and N2O emissions from microcosms in a freshwater marsh in Sanjiang Plain, Northeast China. From July to September in 2005, CO2, CH4 and N2O emission rates were measured in an undisturbed natural marsh (in natural) and microcosms of three manipulated water table treatments: a reference, a high water table (HW) and a low water table (LW). The averages of CO2, CH4 and N2O emissions were 360.2 mg m−2 h−1, 7.43 mg m−2 h−1 and 12.84 μg m−2 h−1, respectively, close to those in reference (p &lt; 0.05), averaging 394.5 mg m−2 h−1, 8.92 mg m−2 h−1 and 13.3 μg m−2 h−1. This means microcosm installation had no significant effect on CO2 efflux. Averaged CO2 (p = 0.03) and CH4 (p = 0.001) emissions were significantly different across the treatments, but that of N2O emission (p = 0.36) was not. To quantify the effects of water table position, three typical classes of water table were considered, i.e. +2 to +14 cm, –11 to 0 cm and −28 to −11.3 cm (+, above the soil surface. –, below the soil surface). Mean CO2 and N2O emissions were lowest at the higher water table positions (+2 to +14 cm) and increased by 120% and 60% at the lower water table positions (−11 to 0 cm), respectively, and the corresponding CH4 emissions decreased by 75%. However, at lowest water table positions (−28 to −11.3 cm), little additional effects on gas emissions were not found. Our results suggested that there could be considerable changes of greenhouse emissions as a response of water drawdown due to wetland drainage. ► Three manipulating water table levels were successfully conducted in a marsh. ► Gas emissions had differences at different water table positions. ► CO2 and N2O emissions were higher when water table below the soil surface. ► CH4 emission were higher when water table above the soil surface. ► There were considerable changes of gas emissions as a response of water drawdown.</abstract><cop>Amsterdam</cop><pub>Elsevier Ltd</pub><doi>10.1016/j.soilbio.2013.02.009</doi><tpages>9</tpages></addata></record>
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source Elsevier ScienceDirect Journals Complete
subjects Agronomy. Soil science and plant productions
Biochemistry and biology
Biological and medical sciences
Carbon dioxide
Chemical, physicochemical, biochemical and biological properties
drainage
drawdown
freshwater
Fundamental and applied biological sciences. Psychology
gas emissions
greenhouse gases
high water table
Marsh
marshes
Methane
Microcosm
Nitrous oxide
Physics, chemistry, biochemistry and biology of agricultural and forest soils
soil
Soil science
Water table
title Effect of water table level on CO2, CH4 and N2O emissions in a freshwater marsh of Northeast China
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