1. 北京师范大学地理学与遥感科学学院
2. 中国科学院水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室
纸质出版:2012
移动端阅览
朱良君, 张光辉, 任宗萍. 4种土壤入渗测定方法的比较[J]. 水土保持通报, 2012,31(6):163-167.
ZHU Liang-jun, ZHANG Guang-hui, REN Zong-ping. Comparing Four Methods for Soil Infiltration Measurement[J]. Bulletin of Soiland Water Conservation, 2012, 31(6): 163-167.
入渗是土壤的基本物理性状
与降雨产流、侵蚀、非点源污染等过程密切相关
快速、准确测定土壤入渗速率具有重要的意义。以黄土高原沟壑区安塞水土保持综合试验站大豆地的黄土为测试土壤
利用双环、单环、圆盘入渗仪、Hood入渗仪4种方法测定了土壤入渗性能
并以双环法测定的稳渗速率、Hood仪测定的饱和导水率、单环/双环和圆盘测定的累积入渗量为基础
比较分析了4种方法各自的优劣。结果表明
单环、圆盘、Hood测定的稳渗速率分别为双环的116%
111%和225%
双环、单环、圆盘测定的饱和导水率分别为Hood的65.8%
75.1%和105%
双环、单环、圆盘达到稳渗时间分别为100
80和30min。说明圆盘测得的稳渗速率、饱和导水率最接近标准值
而且省时省力省水
更适合于野外实验。
Infiltration
as one of the fundamental physical properties
is closely related to many processes including rainfall-runoff
soil erosion and non-point pollution.It is critical to measure soil infiltration rate quickly and accurately.Soil infiltration rates were measured using four methods of double-ring
single-ring
disc permeameter
and Hood infiltrometer on the loess-derived soil with planted soybean at the Ansai Research Station of Soil and Water Conservation
which is located in the hill-gullied area of the Loess Plateau.The results were evaluated based on the measured steady infiltration rate by double-ring method and saturated conductivity by Hood infiltrometer.The results showed that the steady infiltration rates of single-ring
disc
and Hood methods were 116%
111%
and 225% of that of double-ring method
respectively.The saturated conductivities of double-ring
sing-ring
and disc method were 65.8%
75.1%
and 105% of that of Hood method
respectively.The times of reaching the steady infiltration were quite different
approximately 100
80
and 30 minutes for double-ring
single-ring and disc method
respectively.The disc permeameter was more suitable to measure soil infiltration on hillslope for not only the savings in time
labor and water
but also the accuracy in estimating the steady infiltration rate and saturated conductivity.
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