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Effect of Land Use on Soil Properties in Debris Flow Bottomland: A Case Study at Xiaojiang Basin, Yunnan

机译:泥石流底层土地利用对土壤性质的影响-以云南小江盆地为例

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摘要

In order to understand the effect of different land use on soil physics and nutrients properties of the debris flow bottomland, a case study at Daqing gully (in Xiaojiang Basin, Yunnan) was conducted in 2004. Soil samples were taken at depth of 0-10,10-20,20-40,40-60,60-80 cm under three land use patterns crop bottomland ( CL), forest bottomland (FL), and barren bot-tomland(BL). The results showed that the developing bottomland to CL promoted soil toaccumulate total phosphorus (TP) and available phosphorus (AP), pH value transferred from neutral to alkalescency, and organic matter decreased significantly. Furthermore, the contents of total nitrogen (TN) and available nitrogen (AN) in CL were lower than that of FL and BL because the growth of crops consumed more nutrients in soil. The results also showed that the contents of TP, AP and available potassium (AK) in soil were positively correlated with soil particle.
机译:为了了解不同土地利用方式对泥石流底层土壤的物理性质和养分特性的影响,于2004年在云南省小江盆地大庆沟进行了案例研究。在0-10深度采集了土壤样本,10-20,20-40,40-60,60-80 cm在三种土地利用模式下分别为作物低地(CL),森林低地(FL)和荒芜的bottom-land(BL)。结果表明,CL向发育中的低地促进了土壤中总磷(TP)和有效磷(AP)的积累,pH值从中性转移到碱度,有机质显着下降。此外,CL中的总氮(TN)和有效氮(AN)含量低于FL和BL,因为农作物的生长消耗了土壤中更多的养分。结果还表明,土壤中TP,AP和有效钾(AK)的含量与土壤颗粒呈正相关。

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