泾河,Jinghe River
1)Jinghe River泾河
1.The degradation characteristic of organic pollutants in theJinghe River;泾河下游可降解污染物的自净特征
2.Discussion on Leakage in Calcareous Rock Dam Site of Dongzhuang Reservoir ofJinghe River;论泾河东庄水库灰岩坝址渗漏问题
3.Frequency combination method and its application in drought frequency analysis——A Case ofJinghe River;频率组合法及其在干旱频率分析中的应用——以泾河流域干旱频率分析为例
英文短句/例句
1.Piers Stability Analysis of Jing He Continuous Rigid Frame Bridge泾河多跨连续刚构桥桥墩稳定性分析
2.On Analysing the Grain Size Characteristics of Modern Extreme Flood Sediment Trace in Jinghe River Basin泾河流域现代洪水泥痕粒度特征分析
3.Assessment and Analysis on the Ecological Security in the Middle and Lower Reaches of the Jinghe River Basin泾河流域中下游生态安全评价与分析
4.With500 tonnage traffic capacity, Zhangjing River is a golden line for water transport.张泾河通航能力达500吨，是水上运输的“黄金要道”。
5.Analysis of Water and Sediment Reduction Effects by Soil and Water Conservation Treatments in Jing River Basin泾河流域水土保持措施减水减沙作用分析
6.Holocene Environmental Change of Pedogenensis in the Middle Reaches of the Jinghe River Basin;泾河中游地区全新世成壤环境演变研究
7.Micromorphological Features of the Cultivated Soils in the Middle Reaches of the Jinghe River;泾河中游地区耕作土壤的微形态特征研究
8.Studies on the Wild Fire and the Pedogenical Environment Changes of Holocene in the Middle Reaches of the Jinghe River;泾河中游全新世野火与成壤环境变化研究
9.The Study on City Location of An-ding Prefecture and Its Belonging County at Jing River upper and Middle Reaches in Han Dynasty;泾河中上游汉安定郡属县城址及其变迁研究
10.Relationship between land use space difference and driving factors in Jinghe River Basin;泾河流域土地利用区域分异与驱动力的关系
11.Strategy of ecological construction and sustainable agriculture pevelopment of Jinghe Basin;泾河流域生态建设与可持续农业发展对策
12.Land-Use Change Dynamics, Driving Forces and Policy Implications in Jinghe Watershed of Western China;泾河流域土地利用变化驱动力及其政策的影响
13.Spatio-Temporal Changes of Land Use in Jinghe Watershed;泾河流域土地利用格局的时空变化分析
14.Sedimentological characteristics of mud cracks of the modern flood deposit in Jinghe River basin泾河流域现代洪水泥痕沉积学特征研究
15.Planning and Design in Multi-perspective for the Bailianjing Riverfront of the Shanghai World Expo上海世博园区白莲泾河地区多视角规划设计
16.Waist-pit Tombs In Jing River Basin During Western Zhou Dynasty And Qin Ethnic Origin西周时期泾河流域的腰坑墓与秦族起源
17.Flood Discharges Reconstructed by Flood Level Marks on Cliff Faces in Middle Reaches of Jinghe River泾河中游现代洪水痕迹调查对实测洪水的校核
18.Palaeoflood Occurrence in the Late Period of the Longshan Culture in the Middle Reaches of the Jinghe River泾河中游龙山文化晚期特大洪水水文学研究
相关短句/例句
Jing River泾河
1.Speciality researching on water quality of theJing River and the Wei River;泾河和渭河的水质特征研究
2.According to hydrographic data, the average runoff volume ofJing River (from 1932 to 1997)is only half of that of Wei River (from 1950 to 1997), but the suspended sediment ofJing River is 2.泾河年均径流量仅为渭河的 １/２ 倍（资料截止１９９７），输沙量却为渭河的 ２。
3)Jinghe watershed泾河流域
1.Study on land-cover pattern ofJinghe watershed in Loess Plateau;黄土高原泾河流域土地覆被格局研究
2.Structure adjustment of regional water resources based on ecological water requirement of vegetation——A case study in Jinghe Watershed;基于植被生态需水的区域水资源结构调整——以泾河流域为例
3.Water Demand of Crop Plantation in Northwest China——A Case Study of the Jinghe Watershed.;西北地区种植业需水分析——以泾河流域为例
4)Luojing Reach罗泾河段
5)the lower reaches of the Jinghe river泾河下游
1.This paper puts forward some solutions to the serious disasters of landslides visiting the southern-bank ofthe lower reaches of the Jinghe river,which is based on an introduction to the characteristics of landslides,the classification of tableland slopes through calculating the stability coefficient,and a through analysis on the paroxysmal and short-term variable causes for landslides.泾河下游南岸台塬边坡的滑坡灾害严重,本文中分析了滑坡的特征,通过计算边坡稳定性系数对台塬边坡进行了分类,对具有突发性和短期可变性的滑坡触发因素进行了分析,提出了滑坡治理的方法。
6)Jin river basin泾河流域
1.In the next place,on the basis of dynamic water balance simulation ofJin river basin based on the GRID,the natural water renewability .其次,在基于GRID的泾河流域水量动态平衡模拟基础上,通过逐网格计算泾河流域1996年各月水资源自然更新率,来对泾河流域1996年水资源自然再生能力进行评价。
延伸阅读
泾河泾河黄河的三级支流。在中国陕西省中部。源出宁夏回族自治区南部六盘山东麓，有南北两源：南源出泾源县老龙潭，北源出固原大湾镇，两源流至甘肃省平凉市八里桥汇合，东南流经泾川，于杨家坪进入陕西长武县，东南流到高陵县陈家滩汇入渭河。全长455.1千米，流域面积4.54万平方千米。支流众多，主要有马莲河、蒲河、黑河、马拦河、泔河等。流域年平均降水量550毫米，主要集中在夏季。径流年内分配不均匀，洪、枯水流量相差悬殊，1933年8月5日张家山站最大洪水流量9200立方米/秒，1977年4月15日最小流量只有1.94立方米/秒。多年平均年径流量24.4亿立方米。流域内水土流失严重，年平均含沙量141千克/立方米，最大含沙量1430千克/立方米。古人说“泾浊渭清”，只从相对意义上说泾河含沙量比渭河含沙量高。中华人民共和国建立后，对泾河流域进行了治理、开发，上、中游修筑水库和开展大规模水土保持工作，下游开挖和扩建渠道工程。泾惠渠改建了渠首大坝，增加了引水量，扩大了下游灌溉面积。
