Tang Keli,Hou Qingchun,Wang Binke,et al.The Environment Background and Administration Way of Wind-water Erosion Crisscross Region and Shenmu Experimental Area on the Loess Plateau[J].Research of Soil and Water Conservation,1993,(02):2-15.
黄土高原水蚀风蚀交错带和神木试区的环境背景及整治方向
- Title:
- The Environment Background and Administration Way of Wind-water Erosion Crisscross Region and Shenmu Experimental Area on the Loess Plateau
- Keywords:
- loess plateau; water-wind erosion crisscross region; Shenmu experimental area; fragile ecological; environment; environmental administration
- 摘要:
- 黄土高原土壤侵蚀最强烈地区出现于年降水量为400mm左右的水蚀风蚀交错地带，本区气候变化剧烈，植被稀疏，土壤侵蚀全年进行，为典型的脆弱生态环境区。春季风蚀强烈，夏秋暴雨侵蚀频繁，两者交替进行，相互促进，年均侵蚀模数多在10000t/km2以上，境内的晋陕蒙煤田开发区为强烈侵蚀的中心，又为黄河下游河床粗泥沙的主要来源区。鉴于治黄和煤田开发的紧迫需要，神木试区即设于该地区，建立该试区进行环境整治的试验示范研究具有广泛的实际指导意义。综合分析神木试区的优势和劣势。以小流域为单元，探讨工副业与农业相结合，生态效益与经济效益同步发展，农林牧副业生产走向商品化，走向市场的新途径。
- Abstract:
- The most serious soil erosion in the loess plateau exists in the wind-water erosion crisscross region where the annual precipitaton is about 400mm. It is the typic fragile ecologic environment region showing that the climate change is very violent, the vegetation is very scattered and the soil erosion occurs in the whole year. In spring the wind erosion is very serious and in the summer and autumn the storm erosion is very frequent, wind erosion and water erosion occur alternatively and accelerate, which makes the erosion modulus above 10000t/km2·a. The area connecting the Shanxi, Shaanxi, Inner Mongolia and including the Shenmu experimental area is the most serious erosion centre of this region and main source of the coarse sediments of the Yellow River. In view of the urgency of the controlling Yellow River and the coal field development the Shenmu experimental area establishment for envionmental administration experimentdemonstration research has the extensive practical directing significance. By the comprehensive analyzing the superiority and inferiority and taking the small watershed as the unit it is discussed that new way of industry-subsidiary and agriculture combination, simultaneous development, of ecological and economic benefit agriculture forestry and animal husbandry are going forward to the commercialized and marketed.
参考文献/References:
[1] 钱宁等.黄河中游粗泥沙来源区来水来沙对黄河下游的影响.第一次河流泥沙国际学术讨论会论文集,北京:水利出版社,1981
[2] 龚时阳等.黄河泥沙来源与输移.第一次河流泥沙国际学术讨论会文集,北京:水利出版社,1981
[3] 中科院黄考队、唐克丽等.黄土高原地区土壤侵蚀区域特征及其治理途径.中国科学技术出版社,1990
[4] Tang Keli zhang Pingcang and the 1991,Soil Erosion Charaeterisfies and Ecoenvirouman Changes of Water and Wind Erosion Region in the Loess Plaheaa China,Proc of Infer Symp on EnviyonmwfalConfrol and Resourees Ikvelopmwt on Chnas Loess Plates Region Beijing-xian
[5] J. A Eddy,1991 .Arid Ernsysfews Interaetins work shop on RecommendafionFor Drylands Researeh in the Glolal Change Rescarch Program Boulder Colorde d. s. a
[6] 陕西师范大学地理系"陕西省地区地理志"编写组.陕西省榆林地区地理志.陕西人民出版社,p160-168
[7] 唐克丽、杨根生等.晋陕蒙煤田开发区风沙与水土流失灾害及防治对策.中国然灾情分析与减灾对策,中科院地学部主编,湖北科学技术出版杜,1992,P359-368
相似文献/References:
[1]白桦,穆兴民,王双银.水土保持措施对秃尾河径流的影响[J].水土保持研究,2010,17(01):40.
BAI Hua,MU Xing-min,WANG Shuang-yin.Impact of Soil and Water Conservation on River Flow of Tuwei River[J].Research of Soil and Water Conservation,2010,17(02):40.
[2]杨国安,徐勇,郭腾云.基于脆弱性和可持续生计视角的黄土高原生态环境治理研究[J].水土保持研究,2010,17(02):64.
YANG Guo-an,XU Yong,GUO Teng-yun.Eco-environmental Construction on the Loess Plateau Based on the Perspective of the Vulnerability and Sustainable Livelihoods Approaches[J].Research of Soil and Water Conservation,2010,17(02):64.
[3]肖培青,姚文艺,张海峰.黄土高原植被固土减蚀作用研究进展[J].水土保持研究,2012,19(06):282.
XIAO Pei-qing,YAO Wen-yi,ZHANG Hai-feng.Research Progress of the Role of Vegetation in Soil Conservtion and Soil Erosion Reduction on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):282.
[4]马芹,张晓萍,万龙,等.黄土高原河龙区间最大日雨量(PMP)极值拟合及时空演变特征[J].水土保持研究,2012,19(02):71.
MA Qin,ZHANG Xiao-ping,WAN Long,et al.Fitting of the PMP Values and Identifying Its Spatiotemporal Characteristics in the Helong Section on the Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):71.
[5]卓玛兰草,刘普幸,张亚宁,等.甘肃黄土高原区潜在蒸散量时空变化与成因研究[J].水土保持研究,2012,19(01):70.
ZHUO Malancao,LIU Pu-xing,ZHANG Ya-ning,et al.Study on Temporal and Spatial Changes of the Potential Evapotranspiration and Its Impact Factors in Loess Plateau of Gansu Province[J].Research of Soil and Water Conservation,2012,19(02):70.
[6]施宇,温仲明,龚时慧,等.黄土丘陵区植物功能性状沿气候梯度的变化规律[J].水土保持研究,2012,19(01):107.
SHI Yu,WEN Zhong-ming,GONG Shi-hui,et al.Trait Variations along a Climatic Gradient in Hilly Area of Loess Plateau[J].Research of Soil and Water Conservation,2012,19(02):107.
[7]穆兴民,陈国良,徐学选.黄土高原降水量与地理因素关系分析[J].水土保持研究,1992,(02):80.
Mu Xingmin,Chen Guoliang,Xu Xuexuan.ANALYSIS OF THE RELATIONSHIP BETWEEN PRECIPITATION AND GEOGRAPICAL FACTORS IN LOESS PLATEAU[J].Research of Soil and Water Conservation,1992,(02):80.
[8]刘静.数字化地形模型（DTM）在水土保持中的应用[J].水土保持研究,1992,(02):96.
Liu Jeng.ESTABLSHING AND APPLICATION OF DTM FOR SOIL AND WATER CONSERVATION[J].Research of Soil and Water Conservation,1992,(02):96.
[9]侯庆春.神木试区自然条件及环境整治综合分析[J].水土保持研究,1993,(02):136.
Hou Qingchun.Comprehensive Analysis on Natural Conditions and Environmental Harnessing in the Experimental Area[J].Research of Soil and Water Conservation,1993,(02):136.
[10]赵安成.陇东黄土高原沟壑区典型小流域治理模式剖析[J].水土保持研究,1994,1(01):45.
Zhao Ancheng.Analysis of Control Models of Typical Small Watershedin Gully Area of Loess Plateau, the East Part of Gansu Province[J].Research of Soil and Water Conservation,1994,1(02):45.
[11]唐克丽.黄土高原水蚀风蚀交错带小流域治理模式探讨[J].水土保持研究,1996,3(04):46.
Tang Keli.Discussion on Comprehensive Control of Small Watershed in Water and Wind Crisscrossed Erosion Region on The Loess Plateau[J].Research of Soil and Water Conservation,1996,3(02):46.
[12]陈国建,张晓萍,张平仓,等.基于RS和GIS的六道沟流域土地利用动态变化研究[J].水土保持研究,2009,16(02):95.
CHEN Guo-jian,ZHANG Xiao-ping,ZHANG Ping-cang,et al.Dynamic Changes of Land Use in Liudaogou Watershed Based on RS and GIS[J].Research of Soil and Water Conservation,2009,16(02):95.
备注/Memo
收稿日期:1993-10-6