首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms
【2h】

The Spatial Distribution Characteristics of Soil Organic Carbon and Its Effects on Topsoil under Different Karst Landforms

机译:不同岩溶地貌下土壤有机碳的空间分布特征及其对表土的影响

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

Karst landforms are widely distributed in Guizhou Province, and the karst terrain is complex. To investigate the spatial distribution characteristics of soil organic carbon (SOC) in topsoil in different karst landforms, a total of 920 samples were taken from different karst landforms. The study areas, Puding, Xingyi, Guanling, Libo and Yinjiang in Guizhou Province, represent the karst plateau (KP), karst peak-cluster depression (KPCD), karst canyon (KC), karst virgin forest (KVF) and karst trough valley (KTV) landforms, respectively. The characteristics of the SOC contents in areas with different vegetation, land use and soil types under different karst landforms were analyzed. The dimensionality of the factors was reduced via principal component analysis, the relationships among SOC content and different factors were subjected to redundancy analysis, and the effects of the main impact factors on SOC were discussed. The results showed that there was a large discrepancy in the SOC contents in the topsoil layers among different types of karst landforms, the changes in the SOC content in the topsoil layer were highly variable, and the discrepancy in the upper soil layer was higher than that in the lower soil layer. The SOC contents in the 0–50 cm topsoil layers in different karst landforms were between 7.76 and 38.29 g·kg , the SOC content gradually decreased with increasing soil depth, and the descending order of the SOC contents in different karst landforms was KTV > KVF > KC > KPCD > KP.
机译:贵州省岩溶地貌分布广泛,岩溶地形复杂。为了研究不同岩溶地貌表层土壤有机碳的空间分布特征,共采集了920个不同岩溶地貌样品。研究区为贵州省的普定,兴义,关岭,荔波和银江,分别代表了喀斯特高原,喀斯特峰丛洼地,岩溶峡谷,原始森林和喀斯特谷地。 (KTV)地貌。分析了不同岩溶地貌下不同植被,土地利用和土壤类型的土壤有机碳含量特征。通过主成分分析降低了因子的维数,对SOC含量与不同因子之间的关系进行了冗余分析,并讨论了主要影响因子对SOC的影响。结果表明,不同类型的岩溶地貌中表层土壤SOC含量差异较大,表层土壤SOC含量变化变化较大,上层土层差异较大。在较低的土壤层。不同岩溶地貌0-50 cm表层土壤SOC含量在7.76〜38.29 g·kg之间,随着土壤深度的增加,SOC含量逐渐降低,不同岩溶地貌SOC含量的降序为KTV> KVF > KC> KPCD> KP。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

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