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坡耕地反坡水平阶对土壤水N、P垂直再分配的影响

杨绍兵 王克勤 陈志中 康龙

中国水土保持科学2011,Vol.9Issue(1):56-60,73,6.
中国水土保持科学2011,Vol.9Issue(1):56-60,73,6.

坡耕地反坡水平阶对土壤水N、P垂直再分配的影响

Effect of horizontal stage on vertical redistribution of the soil water N and P Oil the sloping land

杨绍兵 1王克勤 1陈志中 2康龙2

作者信息

  • 1. 西南林学院环境科学与工程系,650224
  • 2. 昆明市水务局,650231,昆明
  • 折叠

摘要

Abstract

Combined field observation and laboratory experiment, the Nitrogen and Phosphorus in the soil water of horizontal stage in water source area of Songhuaba reservoir in Kunming were analyzed. The results indicated that TN, NH4+-N, NO3--N and TP had significant difference in the soil water of two treatments in soil layer from 20 cm to 40 cm, TN and NH4+-N had significant difference from 40 cm to 60 cm. The four nutrient mentioned of soil water hadn' t significant difference in two treatments, but hadn't significant difference from 60 cm to 100 cm. In soil layer from 20 cm to 40 cm, the correlation coefficients of TN, NH4+-N concentration of soil water and TN content of soil were 0. 94 ( P < 0.05 ) and 0.97 ( P <0.01 ), and the correlation coefficients of TP concentration of soil water and TP, AP content of soil were 0.90(P <0. 05) and 0. 98(P <0.01 ). The correlation coefficient of TN concentration of soil water and TN content of soil was 0. 92 (P < 0.05 ), and the correlation coefficient of TP concentration of soil water and AP content of soil was 0. 96 (P < 0.01 ) in soil layer from 40 cm to 60 cm. The correlation coefficients of NO3--N concentration of soil water and TN, AN content of soil were 0. 90 (P < 0.05 ) and 0. 92 ( P < 0. 05 ), and the correlation coefficient of TP concentration of soil water and AP content of soil was 0.93 (P < 0. 05 ) in soil layer from 60 cm to 80 cm. The correlation coefficient of NO3--N concentration of soil water and AN content of soil was 0. 94 ( P < 0.05 ) in soil layer from 80 cm to 100 cm. Results show that runoff of the sloping land could change effectively into subsurface flow by reverseslope terrace, N and P concentration of soil water tended to increase in varying degrees in soil layer from 20 cm to 100 cm. Accumulation of N and P of soil were caused by the movement of N and P in soil layers.

关键词

反坡水平阶/土壤水/养分/垂直再分配

引用本文复制引用

杨绍兵,王克勤,陈志中,康龙..坡耕地反坡水平阶对土壤水N、P垂直再分配的影响[J].中国水土保持科学,2011,9(1):56-60,73,6.

基金项目

国家自然科学基金项目"微区域集水系统控制云南山区农业面源污染"(30660037) (30660037)

云南省自然科学基金项目"微区域集水系统控制山区农业面源污染控制"(2006D0041M) (2006D0041M)

云南省科技计划项目"松华坝环境保护域污染综合治理技术"(2006SG20) (2006SG20)

中国水土保持科学

OACSCDCSTPCD

2096-2673

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