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不同母质发育水稻土N2O消耗潜力及环境影响因素

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土壤是N2O的源和汇,在淹水和厌氧条件下具有消耗N2O的能力。稻田土壤长期处于淹水状态,为N2O的消耗提供了有利的环境,从而减少了N2O排放。目前,有关稻田土壤N2O排放的相关研究已有很多,但关于稻田表层土壤N2O的消耗能力及其与环境因素之间的关系研究较少。研究采集了第四纪红壤母质发育的壤土、湖积物砂土发育的砂质壤土、冲积土发育的粉砂质黏壤土 3 类土壤的各 3 个表层(0~5 cm)水稻土,风干后将其回填至具有 5 cm深土柱的培养装置内,在土柱底部添加N2O和添加氦气(He,对照)两个处理,于 28℃下恒温淹水厌氧培养 96 h。培养期间监测各土壤N2O、N2 的动态变化,以及培养前后土壤养分的变化,量化N2O消耗量和N2 增量,以期揭示稻田表层土壤N2O的消耗能力及其与环境因素之间的关系。结果表明,土壤剖面积累的N2O有95。01%~99。92%被稻田表层土壤吸收,其中被还原为N2 的N2O量占总消耗量的 64。50%~83。64%,表明淹水厌氧状态下,不同的水稻土均具有很强的N2O吸收和消耗能力。研究还发现,3 类土壤N2O的消耗存在一定差异,其中影响砂质壤土N2O消耗的主要环境因子为土壤砂粒含量,且两者之间存在显著的线性相关关系(R2=0。964,P=0。000);土壤黏粒、粉砂粒、pH是粉砂质黏壤土N2O消耗的主要环境影响因素,其中土壤黏粒与其消耗量呈显著线性相关(P<0。05);土壤速效钾和铵态氮增加量是影响壤土N2O消耗的主要环境因子,其消耗量与速效钾之间在 0。01 水平上显著正相关。这些结果表明,土壤可溶性有机碳、土壤质地、土壤速效钾等是影响稻田土壤N2O消耗的重要环境因子,且不同土壤N2O消耗的环境影响因子存在差异,这将为调节土壤N2O排放提供重要参考。
Consumption potential of N2O and its influencing factors in paddy soils with different parent materials
Soil is a source and sink of N2O and can consume N2O under flooded and anaerobic conditions.Long-term flooding of paddy soil provides a favorable environment for N2O consumption,thereby reducing N2O emissions.N2O emissions from paddy soils have been studied extensively,but research on the N2O consumption capacity of paddy surface soil and its relationship with environmental factors is still lacking.In this paper,three types of paddy surface soils developed from quaternary red soil(loam,L),lake sediment sand(sandy loam,SL),and alluvial soil(silty clay loam,SCL)were selected to study their N2O consumption capacity using a microcosm experiment(60%soil mass water content and anoxic conditions).Air-dried soils collected from 5 cm in depth were treated with N2O addition(N2O)or helium addition(control)and incubated for 96 h at 28℃.The dynamics of N2O and N2,as well as the changes in soil nutrients during cultivation were monitored.N2O total consumption and N2 production were quantified to explore the consumption capacity of N2O of the three types of paddy soils and their related factors.The paddy surface soils consumed 95.01%-99.92%of the N2O in 5 cm soil depth,and the amount of N2O reduced to N2 was 64.50%-83.64%of the total N2O consumption.This indicated that different paddy soil had strong N2O consumption capacity under flooded and anoxic states.There were significant differences in the N2O consumption among the three soil types.The dominant factor affecting the N2O consumption of SL soils was the soil sand content,with a significant linear correlation(R2=0.964,P=0.000).Soil clay,silt,and pH were the main environmental factors affecting N2O consumption in SCL soils,and soil clay was significantly linearly related to its consumption(P<0.05).Soil available potassium and the increment of ammonium nitrogen was the main factor affecting the consumption of N2O in L soils.There was a significantly positive correlation between consumption and available potassium(P<0.01).Results showed that soil dissolved organic carbon,soil texture,and soil available potassium were important environmental factors affecting N2O consumption in paddy soils.The dominant factors varied for different soil types,which could provide an important reference for regulating N2O emissions from paddy fields.

paddy surface soilsN2O consumptionsoil pHsoil dissolved organic carbonsoil textureflooding and anoxic

杨曼、钟金梅、王薇、赵丽娅、李兆华、李昆、王玲

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湖北省区域发展与环境响应重点实验室,湖北大学,湖北 武汉 430062

湖北省农村安全饮用水工程技术研究中心,湖北 武汉 430062

表层水稻土 N2O消耗 土壤pH 土壤可溶性有机碳 土壤质地 淹水缺氧

国家自然科学基金湖北省区域发展与环境响应重点实验室基金项目湖北省区域发展与环境响应重点实验室基金项目

418070432020A0032021A002

2024

中国土壤与肥料
中国农业科学院农业资源与农业区划研究所 中国植物营养与肥料学会

中国土壤与肥料

CSTPCD北大核心
影响因子:1.197
ISSN:1673-6257
年,卷(期):2024.(4)