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径流小区集流桶含沙量测量方法研究
引用本文:符素华,付金生,王晓岚,刘宝元,袁爱萍.径流小区集流桶含沙量测量方法研究[J].水土保持通报,2003,23(6):39-41.
作者姓名:符素华  付金生  王晓岚  刘宝元  袁爱萍
作者单位:1. 北京师范大学,资源与环境科学系,北京,100875
2. 北京市水土保持工作总站,北京,100037
基金项目:国家自然基金课题(40201031),国家重点基础研究发展规划项目(G2000018602),北京市水土保持监测项目资助
摘    要:径流小区是研究坡面土壤侵蚀的重要观测手段,含沙量的测定是准确计算土壤流失量的关键。用传统方法很难测到粗颗粒,使测到的含沙量明显偏小。试验在密云石匣示范区坡面径流试验小区下面的分流桶内进行,用人工在径流桶内加沙的方法制备约4,12,30,60,90,120kg/m3不同含沙量。然后分别用传统测量方法和改进的分层测量方法进行了粗沙区的含沙量观测,并将观测结果与实际含沙量进行了对比。研究结果表明,传统测量方法所测得的含沙量远小于实际含沙量,平均相对误差为-83.05%;而分层测量所测得的含沙量基本上接近于实际值,平均相对误差为-2.77%。

关 键 词:含沙量  土壤侵蚀  石质山区
文章编号:1000-288X(2003)06-0039-03
收稿时间:2003/1/20 0:00:00
修稿时间:2003年1月20日

Sediment Content Measurement in Collecting Tanks of Runoff Plots
FU Su-hu,FU Jing-sheng,WANG Xiao-lan,LIU Bao-yuan and YUAN Ai-ping.Sediment Content Measurement in Collecting Tanks of Runoff Plots[J].Bulletin of Soil and Water Conservation,2003,23(6):39-41.
Authors:FU Su-hu  FU Jing-sheng  WANG Xiao-lan  LIU Bao-yuan and YUAN Ai-ping
Institution:FU Su-hua~1,FU Jing-sheng~1,WANG Xiao-lan~1,LIU Bao-yuan~1,YUAN Ai-ping~2
Abstract:Runoff plots are very important for soil erosion study. The measurement of sediment content is a key part in the process of soil loss calculation. It is so difficult for traditional measurement method to measure sandy particle that sediment content measured is apparently less than true value. The study was conducted in collecting tank at Shixia watershed, Miyun county of Beijing city. The six different sediment content including about 4, 12, 30, 60, 90, 120 kg/m~3 were put into collecting tank with about 0.7 m deep water, respectively. The traditional measurement method and layered measurement were used to measure sand content. The measurement results of these two methods were compared with true sand content. The results show that traditional measurement method underestimated sand content and the relative difference was (-83.05%), while layered measurement method can precisely measure sand content and the relative difference was -2.77%.
Keywords:sediment content  soil erosion  stony mountainous area
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