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Effects of plant-derived dissolved organic matter (DOM) on soil CO2 and N2O emissions and soil carbon and nitrogen sequestrations

机译:植物来源的可溶性有机物(DOM)对土壤CO2和N2O排放以及土壤碳氮固存的影响

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Dissolved organic matter (DOM) in soils play an essential role in soil physical, chemical and biological processes, but little information is available on the biodegradability of plant-derived DOM and its effect on soil carbon and nitrogen sequestration in field soils. The objectives of this study were to investigate the impacts of crop residue-derived DOM on soil CO2 and N2O emissions, as well as soil carbon and nitrogen sequestration by adding water extracts of maize stalk (i.e., plant-derived DOM) to soils. In this study, wheat was grown in pots under field conditions with treated soils, the soils treatments were: plant-derived DOM (PDOM), urea nitrogen (N), PDOM + urea nitrogen (PDOM + N), as well as a control with no additions to soil (CK). Adding plant-derived DOM to soil increased soil CO2 and N2O emissions (P 0.05). During the wheat growing season, the cumulative CO2-C emission from CK, PDOM, N and PDOM + N was 107 +/- 1, 157 +/- 7, 136 +/- 2 and 149 +/- 6 g Cm-2, respectively. Meanwhile, the cumulative N2O-N emission from CK, PDOM, N and PDOM + N was 188 +/- 8, 256 +/- 5, 239 +/- 10 and 258 +/- 7 mg N m(-2), respectively. Compared with N treatment, DOM addition had little effect on soil N sequestration, but it accelerated the decomposition of native soil organic carbon (SOC) and caused a net loss of SOC. The soil C sequestration decreased about 151 +/- 67 and 51 +/- 45 g C m(-2) in PDOM and PDOM + N treatments, respectively. The increased microbial biomass and root biomass were responsible for the greater CO2 emission in DOM-amended soils. Negative correlation between dissolved organic carbon (DOC) content and N2O flux suggested that the release of N2O was dependent on the supply of DOC. These results indicated that the supply of plant-derived DOM exacerbated soil CO2 and N2O emissions and reduced soil C sequestration. Therefore, agricultural management practices that increase the stability of highly soluble C inputs and/or retard the decomposition of crop residues should be adopted to decrease soil greenhouse gas emission and increase soil C sequestration. (C) 2015 Elsevier B.V. All rights reserved.
机译:土壤中的溶解性有机物(DOM)在土壤物理,化学和生物过程中起着至关重要的作用,但是关于植物来源的DOM的生物降解性及其对田间土壤中碳和氮固存的影响的信息很少。这项研究的目的是通过将玉米秸秆的水提取物(即植物来源的DOM)添加到土壤中来研究农作物残留的DOM对土壤CO2和N2O排放的影响以及碳和氮的固存。在这项研究中,小麦是在田间条件下用处理过的土壤在盆中种植的,土壤处理为:植物来源的DOM(PDOM),尿素氮(N),PDOM +尿素氮(PDOM + N)以及对照不含土壤(CK)。向土壤中添加植物来源的DOM会增加土壤CO2和N2O排放(P <0.05)。在小麦生长期,CK,PDOM,N和PDOM + N累积的CO2-C排放量为107 +/- 1、157 +/- 7、136 +/- 2和149 +/- 6 g Cm-2 , 分别。同时,CK,PDOM,N和PDOM + N累积的N2O-N排放为188 +/- 8、256 +/- 5、239 +/- 10和258 +/- 7 mg N m(-2),分别。与氮处理相比,添加DOM对土壤固氮影响不大,但促进了土壤天然有机碳(SOC)的分解,并导致SOC的净损失。在PDOM和PDOM + N处理中,土壤固碳分别降低了约151 +/- 67 g C m(-2)和51 +/- 45 g C m(-2)。微生物生物量和根系生物量的增加是DOM改良土壤中CO2排放量增加的原因。溶解有机碳(DOC)含量与N2O通量之间呈负相关关系,表明N2O的释放取决于DOC的供应。这些结果表明,植物来源的DOM的供应加剧了土壤CO2和N2O的排放并减少了土壤C的固存。因此,应采用增加高可溶性碳输入的稳定性和/或延缓作物残渣分解的农业管理措施,以减少土壤温室气体的排放并增加土壤中的碳固存。 (C)2015 Elsevier B.V.保留所有权利。

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