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煤矸石山风化堆积物水分动态研究
引用本文:张锐,张成梁,李美生,张洪江,程金花.煤矸石山风化堆积物水分动态研究[J].水土保持通报,2008,28(1):124-129.
作者姓名:张锐  张成梁  李美生  张洪江  程金花
作者单位:1. 中国科学院,山地灾害与地表过程重点实验室,四川,成都,610041;中国科学院水利部成都山地灾害与环境研究所,四川,成都,610041
2. 贵州赤天化纸业股份有限公司,贵州,赤水,564707
3. 中国科学院水利部成都山地灾害与环境研究所,四川,成都,610041
基金项目:水利部中国水土流失与生态安全综合科学考察长江上游及西南诸河考察项目
摘    要:以位于贵州省赤水市的"黔北20万吨/年竹浆林纸一体化工程项目"为例,研究了低山丘陵区开发建设项目中的水土保持和生态建设问题.针对该工程水土流失的现状和特点,结合竹原料林基地建设,提出了水土流失的防治原则和采取的防治对策.实施水土保持方案后,能有效控制工程区的水土流失,恢复和改善项目区的生态环境,保障了工程建设的安全,实现了社会、经济、环境的协调与可持续发展.

关 键 词:低山丘陵区  开发建设项目  水土流失  水土保持  生态建设  低山丘陵区  开发建设项目  水土保持方案  生态建设  Region  Hill  Construction  Project  Development  Reconstruction  Ecological  Water  Conservation  可持续发展  协调  生态环境  经济  社会  安全  工程建设  保障  项目区
文章编号:1000-288X(2008)01-0119-05
收稿时间:2006-10-26
修稿时间:2007-07-11

Research on Water Dynamics of Weathered Coal Gangue Dumps
ZHANG Rui,ZHANG Chengliang,LI Meisheng,ZHANG Hongjiang and CHENG Jinhua.Research on Water Dynamics of Weathered Coal Gangue Dumps[J].Bulletin of Soil and Water Conservation,2008,28(1):124-129.
Authors:ZHANG Rui  ZHANG Chengliang  LI Meisheng  ZHANG Hongjiang and CHENG Jinhua
Institution:College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;Baolv Design and Research Institute of Gardens, Taiyuan, Shanxi 030012, China;Guoyang New Energy Resources Co. , Ltd. , Yangquan, Shanxi 045000, China;College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;College of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China
Abstract:Water dynamics of the 280 coal gangue dumps in Yangquan City,Shanxi Province was preliminarily studied by the analyses of physical properties,water infiltration characteristics,and water contentof the weathered gangue. Results showed thatcoal gangue texture was poor and the average contentof gravel and boulder was as high as 86. 07 %. The coal gangue dumps were dominated by non-capillary pore and the aver age values of capillary pore atthe four depths (15,30,45,and 60 cm) in the profile were 1. 40 %,1. 36 %,1. 32 %,and 1. 17 %,respectively. This caused soil water2holding capacity maintaining ata low-level throughoutthe year and the average water-holding capacity at60 cm depth was 19. 7 t/hm2. Kostiakov infil tration model can well describe the infiltration process of weathered gangue. During the infiltration process,weathered gangue had higher infiltration rate. The seasonal change in water contentof weathered gangue was mainly influenced by the amountof rainfall and its distribution. With the increasing seasonal rainfall,the av erage water contentof weathered gangue rose correspondingly. Water storage of gangue dump was linearly related with the amountof rainfall. When the amountof rainfall was low,or rainfall eventwas highly fre quent,water storage of exposed gangue was more than thatof the gangue dump covered with soil. Generally speaking,there was a dry layer between 30 and 40 cm in gangue dump,which made the lower layers of gangue dump keeping more moisture in dry season.
Keywords:low mountain and hill region  development and construction project  soil and water loss  soil and water conservation  ecological reconstruction
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