韩江流域典型区,typical area of Hanjiang River Basin
1)typical area of Hanjiang River Basin韩江流域典型区
1.By using the research method of field investigation,soil sampling and laboratory analysis,the soil organic carbon storage and nutrients pools for the four main forest types intypical area of Hanjiang River Basin have been discussed.采用野外调查、取样和室内实验分析相结合的方法,研究韩江流域典型区4种主要林分土壤有机碳储量和全量养分库的分布特征。
英文短句/例句
1.Grey Relational Analysis of Soil Fertility of Main Forest Soils in Typical District of Hanjiang River Basin韩江流域典型区主要森林类型土壤肥力的灰色关联度分析
2.A Primary Study on the Soil Properties of the Different Forest in Typical Area of Hanjiang River Basin韩江流域典型区不同森林类型土壤理化性质初步研究
3.Soil Organic Carbon Storage and Nutrients Pools of Several Forest Types in Typical Area of Hanjiang River Basin韩江流域典型区几种森林土壤有机碳储量和养分库分析
4.Study on the Physico-Chemical Properties of Soil Developed from Purple Sandstone(K2yt) in Typical Area of Hanjiang Valley韩江流域典型区叶塘组紫色岩上发育土壤理化性质研究
5.Aircraft Measurement of Air Pollutants over the Typical Regions of the Yangtze Valley;长江流域典型区域空气污染物的航空测量
6.Divided Research of the Eco-hydrology Regionalization in Typical Basin(area) of the upper Reaches of the Changjiang River;长江上游典型流（区）域生态水文区划分的研究
7.DPS-based Study on the Eco-economic Regionalization in the Youjiang River Drainage Basin On the Scale of Town:Taking the Typical Region in the Youjiang River Drainage Basin as an Example基于DPS的右江流域乡镇尺度生态经济区划探讨——以右江流域典型区域为例
8.Runoff Process in a Typical Small Permafrost Watershed at the Headwaters of Yangtze River长江源典型多年冻土区小流域径流过程特征研究
9.Study on Effect of Ecological Restoration in Soil and Water Conservation and Division of Exemplary Area in Middle and Upper Reaches of ChangJiang River;长江流域上中游典型区水土保持生态恢复分区及恢复效果研究
10.Hydrological Process in a Typical Small Permafrost Watershed at the Headwaters of Yangtze River长江源多年冻土区典型小流域水文过程特征研究
11.Benefit of Soil and Water Conservation at a Typical Basin of the Upper Reaches of Yangtze River长江上游典型流域水土保持效益分析
12.Study on the Soil Physical & Chemical Properties and the Water Conservation Function of the Different Forest in Meijiang District韩江流域梅江区林地土壤理化性质及水源涵养能力
13.Study on Land Use/Cover Change in Typical Areas of Yongding River Watershed永定河流域典型区土地利用/覆被变化
14.Society economy evaluation of typical karst cell in Lijiang River basin;漓江流域典型岩溶单元社会经济状况评价
15.ECOLOGICAL EVALUATION ON LAND CONSOLIDATION IN TYPICAL KARST WATER BASIN--A Case Study in Xiaojiang Water Basin in Yunnan Province;典型岩溶流域土地整理的生态评价——以云南小江流域为例
16.Land Use Change in Typical Karst Watershed Using GIS-based Analysis--Taking Xiaojiang Watershed of Yun nan Province as an Example;基于GIS的典型岩溶流域土地利用变化分析——以云南省小江流域为例
17.A Study on the Land Use/Land Cover Change and Driving Mechanism in the Typical Region of Yiluo River Drainage Basin;伊洛河流域典型区域LUCC及其驱动机制研究
18.New Viewpoint on the Cause of Crocodile’s Extinction in Han River Valley;历史时期韩江流域鳄鱼灭绝原因新探
相关短句/例句
Hanjiang River Basin韩江流域
1.Guideline and Emphasis ofHanjiang River Basin Water Quantity Allocation Study;韩江流域水量分配方案的研究思路与研究重点
2.Grey Relational Analysis of Soil Fertility of Main Forest Soils in Typical District ofHanjiang River Basin韩江流域典型区主要森林类型土壤肥力的灰色关联度分析
putation of Probable Maximal Precipitation and Flood with Rainstorm Displacing inHanjiang River Basin韩江流域可能最大暴雨洪水移置计算
3)Typical Basin(area)典型流(区)域
1.Divided Research of the Eco-hydrology Regionalization in Typical Basin(area) of the upper Reaches of the Changjiang River;长江上游典型流（区）域生态水文区划分的研究
4)Hanjiang River Basin Guangdong province广东韩江流域
5)typical region典型区域
6)typical watershed典型流域
1.Research ontypical watershed eco-hydrological process and its synergistic changes based on land cover/ land change (LUCC) has an impo.借助WEPP模型提取研究区代表性典型流域单元并对其径流及侵蚀产沙进行模拟;基于分形理论测算典型流域单元地形地貌特征分形维数,建立流域水沙运移与地貌形态耦合关系;根据自相似原理,在考虑降雨异质性基础上建立流域泥沙输移比的尺度转换模型;结合流域地形地貌、土地利用格局、降水信息,建立了描述时空变异性、多变量的耦合水文模型,探讨流域不同时、空尺度上水沙运移的转换方法。
延伸阅读
韩江韩江位于中国广东省东部。上游有两源：北源汀江，又名鄞江，发源于福建省长汀县东北上坪山，自北向南流。南源梅江发源于广东省紫金县白山东，自南向北偏东流。两江在大埔县三河坝汇合后始称韩江，南流到澄海市分成东、西、北3支，由5个口门流入南海，全长428千米，流域面积3万平方千米。梅江和汀江从各自源头到三河坝分别长为300千米和260千米，由于梅江河长大于汀江，故多将梅江作为韩江的正源。汀江属山溪性河流，多峡谷、险滩，径流丰富，多年平均径流深965毫米（溪口站）。梅江蜿蜒于广谷和盆地中，多年平均径流深760毫米（横山站）。韩江流域水力资源理论蕴藏量为201.44万千瓦，实际可开发量为142万千瓦，以汀江流域水力资源最为丰富。汀江自上杭可上溯通航汽轮50千米；梅江从梅州可以上溯汽轮至五华。梅州以下和韩江可以通2.5～30吨级轮船。
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