用户名: 密码: 验证码:
Using Soil Water Content Sensors to Charac
详细信息   在线全文   PDF全文下载
摘要

Because groundwater is a source of drinking water for many people, there is great concern to protect groundwater resources. Preferential flow through the unsaturated zone is considered one of the main contributory factors in groundwater pollution, which is influenced primarily by soil heterogeneity and management practices. To characterize the degree of preferential flow, the soil water content dynamics during short- and long-term periods in the shallow zone (0–40-cm depth) of two plots with no-till (NT) and conventional tillage (CT) soil management practices were investigated for 2 yr using soil water sensors placed horizontally in a rectangular grid along transects across crop rows. Analysis of response times and water content changes during rainfall events confirmed the existence of short-term preferential flow at the site and that macropores and heterogeneities in soil hydraulic parameters in the shallow zone may have contributed to infiltration into the deeper layers in the NT plot. In the longer term, the pathways of infiltration and redistribution were different between the growing and non-growing seasons; however, these differences were relatively stable in both plots during the 2-yr study period.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700