1) Yuan River
沅江
1.
Analysis of Yuan River water quality with a forecast of TP concentration in Wu Qiangxi Reservoir;
沅江干流水质变化时空规律及五强溪水库库区总磷预测
2.
Application Research of Artificial Neural Network Method on Water Quality Estimation in Yuan River Upriver;
人工神经网络在沅江中上游水环境质量评价中的应用研究
2) Yuanjiang River
沅江
1.
Soil Organic Carbon Loss in the Wujiang River and Yuanjiang River Catchments;
乌江/沅江流域土壤有机碳的丢失
2.
In this paper, the characteristics of wastewater discharged into rivers are analyzed, and the water quality of rivers and tributaries, including the Xiangjiang River, Zishui River, Yuanjiang River, and Lishui River are evaluated.
就湖南省入河废污水的特征与主要河流水质进行分析 ,采取 1 998年监测资料 ,对湘江、资水、沅江、澧水的干支流水质分别进行评价。
3.
Water quality of lower reaches of Yuanjiang River,a rarely studied large river,was sampled and assessed through multiple assessment method and cluster analysis.
采用多重评价方法与聚类分析法对研究很少的大型江河——沅江下游的水质情况开展了调查、分析和质量评价。
3) Yuanjiang
沅江
1.
Investigation on mollusca resources of Southern Dongting Lake in Yuanjiang city;
沅江南洞庭湖软体动物资源初步调查
2.
The Phonological Study of Nandashanzhen Dialects in Yuanjiang;
沅江市南大膳镇话语音研究
4) Yuanjiang City
沅江市
1.
Effects of Sluicing Flood via Plain on Regional Land Use of Dongting Lake Region——Taking Yuanjiang City of Hunan as Example;
洞庭湖区平垸行洪对土地利用结构的影响——以湖南沅江市为例
5) aloe
[英]['æləʊ] [美]['ælo]
沅江芦荟
1.
Karyotype and Giemsa C-bandtype anelysis of aloe(Aguanjanginsis);
沅江芦荟染色体核型和Giemsa C-带带型
6) Yuanjiang sag
沅江凹陷
1.
Using the data obtained from seismic, well log, and assaying, the research is conducted on sequence stratification and sedimentary facies of Taoyuan Formation, Yuanjiang Formation, Hanshou Formation, and Xinhekou Formation of Paleogene inYuanjiang sag in the Dongtinghu Basin.
通过地震、测井和分析化验等资料,对洞庭湖盆地沅江凹陷古近系古新统桃源组及始新统沅江组、汉寿组及新河口组进行层序地层和沉积相研究,首先可将古近纪划分为2个Ⅲ级层序、5个体系域,桃源组和沅江组构成层序I,汉寿组和新河口组构成层序Ⅱ。
2.
The Paleogene in Yuanjiang sag of the Dongting basin occurs as a NE-trending quasi-dustpan-shaped sag being faulted in the southeast and onlapping in the northwest.
洞庭盆地沅江凹陷古近系总体表现为一个北东向展布的东南断裂、西北超覆的断陷—断坳型准箕状凹陷。
补充资料:沅江
沅江 位于中国湖南省西部 。源出贵州省东南部 。分南北两源:南源龙头江,源出都匀市云雾山鸡冠岭;北源重安江,源出麻江县北之大山。两水汇合后称清水江。东流至黔城会沅水后,水量大增,始称沅江。东北流经辰溪县、沅陵县、常德市,在德山入洞庭湖。长1033千米,流域面积8.92万平方千米。河网发育,呈羽状水系。主要支流有沅水、辰水、武水、酉水、渠水、巫水、溆水等。黔城以上为上游,属贵州高原(云贵高原),峰回水转,河道弯曲,水势湍急;黔城至沅陵为中游,滩陡礁多浪险;沅陵以下属下游,山势低落,至桃源河流入平原,江阔波平,舟行通畅。多年平均径流量677亿立方米。水力资源丰富 ,已在酉水中游建成的凤滩电站装机40万千瓦。贵州省天柱县远口镇以下可通航。 |
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