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中国西北边缘绿洲农田转变为苜蓿饲料地后土壤团聚体、碳和氮储量的变化。

Changes in soil aggregate, carbon, and nitrogen storages following the conversion of cropland to alfalfa forage land in the marginal oasis of northwest China.

作者信息

Su Yong Zhong, Liu Wen Jie, Yang Rong, Chang Xue Xiang

机构信息

Laboratory of Watershed Hydrology and Applied Ecology, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, China.

出版信息

Environ Manage. 2009 Jun;43(6):1061-70. doi: 10.1007/s00267-009-9284-x. Epub 2009 Feb 26.

Abstract

Maintenance of soil organic carbon (SOC) is important for sustainable use of soil resources due to the multiple effects of SOC on soil nutrient status and soil structural stability. The objective of this study was to identify the changes in soil aggregate distribution and stability, SOC, and nitrogen (N) concentrations after cropland was converted to perennial alfalfa (Medicago sativa L. Algonguin) grassland for 6 years in the marginal oasis of the middle of Hexi Corridor region, northwest China. Significant changes in the size distribution of dry-sieving aggregates and water-stable aggregates, SOC, and N concentrations occurred after the conversion from crop to alfalfa. SOC and N stocks increased by 20.2% and 18.5%, respectively, and the estimated C and N sequestration rates were 0.4 Mg C ha(-1) year(-1) and 0.04 Mg N ha(-1) year(-1) following the conversion. The large aggregate (>5 mm) was the most abundant dry aggregate size fraction in both crop and alfalfa soils, and significant difference in the distribution of dry aggregates between the two land use types occurred only in the >5 mm aggregate fraction. The percentage of water-stable macroaggregates (>2, 2-0.25 mm) and aggregate stability (mean weight diameter of water-stable aggregates, WMWD) were significantly higher in alfalfa soils than in crop soils. There was a significant linear relationship between total SOC concentration and aggregate parameters (mean weight diameter) for alfalfa soils, indicating that aggregate stability was closely associated with increased SOC concentration following the conversion of crops to alfalfa. The SOC and N concentrations and the C/N ratio were greatest in the >2 mm water-stable aggregates and the smallest in the 0.25-0.05 mm aggregates in crop and alfalfa soils. For the same aggregate, SOC and N concentrations in aggregate fractions increased with increasing total SOC and N concentrations. The result showed that the conversion of annual crops to alfalfa in the marginal land with coarse-texture soils can significantly increase SOC and N stocks, and improve soil structure.

摘要

由于土壤有机碳(SOC)对土壤养分状况和土壤结构稳定性具有多种影响,因此维持土壤有机碳对于土壤资源的可持续利用至关重要。本研究的目的是确定在中国西北河西走廊中部边缘绿洲,农田转变为多年生紫花苜蓿(苜蓿品种阿尔冈金)草地6年后土壤团聚体分布与稳定性、土壤有机碳和氮(N)浓度的变化。从作物转变为苜蓿后,干筛团聚体和水稳性团聚体的大小分布、土壤有机碳和氮浓度发生了显著变化。转变后,土壤有机碳和氮储量分别增加了20.2%和18.5%,估计的碳和氮固存率分别为0.4 Mg C ha(-1) 年(-1) 和0.04 Mg N ha(-1) 年(-1)。大团聚体(>5 mm)是作物和苜蓿土壤中最丰富的干团聚体粒径部分,两种土地利用类型之间干团聚体分布的显著差异仅出现在>5 mm团聚体部分。苜蓿土壤中水稳性大团聚体(>2、2 - 0.25 mm)的百分比和团聚体稳定性(水稳性团聚体的平均重量直径,MWWD)显著高于作物土壤。苜蓿土壤中总土壤有机碳浓度与团聚体参数(平均重量直径)之间存在显著线性关系,表明从作物转变为苜蓿后,团聚体稳定性与土壤有机碳浓度增加密切相关。作物和苜蓿土壤中,>2 mm水稳性团聚体中的土壤有机碳和氮浓度最高,0.25 - 0.05 mm团聚体中的最低。对于相同的团聚体,团聚体组分中的土壤有机碳和氮浓度随总土壤有机碳和氮浓度的增加而增加。结果表明,在质地粗糙的边际土地上,将一年生作物转变为苜蓿可以显著增加土壤有机碳和氮储量,并改善土壤结构。

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