自然科学版
陕西师范大学学报(自然科学版)
资源与环境科学
基于137Cs示踪和WaTEM/SEDEM模型的黑土区小流域侵蚀产沙模拟
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李国强1,2, 方海燕2*
(1 杭州市水文水资源监测总站, 浙江 杭州 310016;2 中国科学院地理科学与资源研究所 陆地水循环及地表过程重点实验室, 北京 100101)
李国强,男,硕士,主要研究方向为土壤侵蚀与水土保持。E-mail: li_gq550@163.com
摘要:
以位于东北典型黑土区的黑龙江省拜泉县双阳河中上游24个水库控制流域为研究对象,将137Cs核素示踪得到的土壤侵蚀强度数据用于WaTEM/SEDEM模型参数的校正,并利用24个水库流域的产沙数据进行验证。齐心水库流域25个不同土地利用土样点的土壤侵蚀强度表明,耕地侵蚀强度大,平均侵蚀强度为24.5 t/(hm2·a),灌木林和草地侵蚀强度居中,平均侵蚀强度分别为5.6和9.5 t/(hm2·a);林地侵蚀强度最小,平均侵蚀强度为1.1 t/(hm2·a)。WaTEM/SEDEM模型校正得到了泥沙输移能力系数(Ktc)最低值和最高值的最佳组合为4 m和8 m,此时模型效率系数cNS达到最大值0.62。对24个水库流域模拟得到的年产沙量和产沙模数与实际产沙相关系数均达0.70以上。此核素示踪技术和模型模拟的有效结合,可为水沙资料稀缺的黑土区或类似地区的土壤侵蚀研究及水土保持合理实施提供理论指导。
关键词:
黑土区; 土壤侵蚀; 核素示踪; 模型; 模拟
收稿日期:
2014-12-27
中图分类号:
S157.1
文献标识码:
A
文章编号:
1672-4291(2015)03-0086-07doi:10.15983/j.cnki.jsnu.2015.03.433
基金项目:
国家自然科学基金资助项目(41271305)
Doi:
Modeling soil erosion and sediment yield in a small catchment of the black soil region using 137Cs technique and WaTEM/SEDEM
LI Guoqiang1,2, FANG Haiyan2*
(1 Hangzhou Hydrology and Water Resources Monitoring Center, Hangzhou 310016, Zhejiang, China; 2 Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China )
Abstract:
Severe erosion of black soil in Northeastern China has attracted great attention, and more work on soil erosion and soil conservation have been conducted in recent years. However, few studies on physical erosion modeling in this region have been conducted. In the study, 24 reservoir catchments in Baiquan county were selected as study objects, and the 137Cs technique was successfully combined with a soil erosion model WaTEM/SEDEM (Water and Tillage Erosion Model and Sediment Delivery Model). The 137Cs-derived soil erosion intensities were used as input data to run and calibrate the WaTEM/SEDEM model firstly, and then the model was validated using the sediment yields from the 24 reservoir catchments. Soil erosion intensity in the cultivated lands is the highest, averaging 24.5 t/(hm2·a), and the mean erosion intensities in shrub and grass lands are 5.6 and 9.5 t/(hm2·a), respectively. The mean erosion intensity in forest lands is the minimum. The optimal combination of the minimum and maximum Ktc values of WaTEM/SEDEM was 4 m and 8 m, with the highest cNS (Nash-Sutcliffe coefficient) of 0.62. The calibrated model has a robust modeling capacity, and the correlation coefficients of the modeled sediment yield(YS) and the specific sediment yield(YSS) and the observed counterparts are both over 0.70 for the 24 reservoir catchments. This study can provide scientific basis for soil erosion study and conservation measures implemented in the black soil region and other similar regions.
KeyWords:
black soil region; soil erosion; nuclear tracing; model; modeling