首页> 外文期刊>Plant and Soil >Degraded vegetation and wind erosion influence soil carbon, nitrogen and phosphorus accumulation in sandy grasslands
【24h】

Degraded vegetation and wind erosion influence soil carbon, nitrogen and phosphorus accumulation in sandy grasslands

机译:植被退化和风蚀影响沙质草地土壤碳,氮和磷的积累

获取原文
获取原文并翻译 | 示例
           

摘要

A field study was conducted in a semi-arid sand land ecosystem in eastern Inner Mongolia, China, to explore the mechanisms underlying how human-induced environmental degradation in sandy grasslands influences ecosystem plant diversity, productivity, soil erodibility, and soil carbon (C), nitrogen (N) and phosphorus (P) accumulation and storage. We investigated (1) C, N and P accumulation to 20cm soil depth; (2) C, N and P storage in plant litter, above- and below-ground biomass; and (3) the rate of surface wind erosion measured as the amount of aeolian soil accumulating in the traps and C, N and P output from the topsoil removal due to wind erosion during the erosive season in four habitats of differently degraded sandy grasslands. Environmental degradation has resulted in significant and differential reductions in soil C, N and P accumulation within the top 20cm soil layer across habitats. On average, the most severely degraded sandy grassland stored 474%, 198% and 56% less soil C, N and P, while the severely degraded sandy grassland stored 215%, 121% and 27% less soil C, N and P and the moderately degraded sandy grassland stored 111%, 60% and 17% less soil C, N and P than did the lightly degraded sandy grassland. Two key variables associated with reduced soil C, N and P accumulation in sandy grasslands as a result of environmental degradation are reduced plant litter and above- and below-ground biomass production (i.e. less plant C, N and P inputs in the soil) and increased C, N and P output from the removal of nutrient-rich topsoil layers resulted from increased rates of wind erosion. This study suggests a complex mechanism by which environmental degradation influences soil C, N and P accumulation and dynamics via its significant effects on ecosystem plant diversity, productivity and soil erodibility.
机译:在中国内蒙古东部的半干旱沙地生态系统中进行了一项野外研究,以探讨人为引起的沙质草地环境退化如何影响生态系统植物多样性,生产力,土壤易蚀性和土壤碳的机制。 ,氮(N)和磷(P)的积累和储存。我们调查(1)碳,氮和磷在20cm土深处的积累; (2)植物凋落物,地上和地下生物量中的碳,氮和磷储量; (3)在四个退化程度不同的沙质草地生境中,以风蚀时期的风蚀土壤为依据,表层风蚀土壤的积聚率是指圈闭中积聚的风积土的数量,以及由于侵蚀造成的表土去除的C,N和P输出。环境退化已导致跨生境的最上层20厘米土壤层中土壤C,N和P积累的显着差异减少。平均而言,退化最严重的沙质草地的土壤碳,氮和磷含量分别减少了474%,198%和56%,而退化程度最严重的沙质草地的碳,氮和磷含量分别降低了215%,121%和27%。中度退化的沙质草地比轻度退化的沙质草地存储的土壤C,N和P减少111%,60%和17%。与环境退化导致的沙质草地土壤C,N和P积累减少相关的两个关键变量是植物凋落物减少和地上和地下生物量生产(即土壤中植物C,N和P投入减少)和去除富含营养的表土层增加的碳,氮和磷产量是由于风蚀速率增加所致。这项研究提出了一个复杂的机制,环境退化通过其对生态系统植物多样性,生产力和土壤易蚀性的显着影响,影响土壤碳,氮和磷的积累和动态。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号