gaocun meaning in Chinese
高村
Examples
- The river section from tieshu , mengjin , henan province to gaocun , shandong provice , is a wandering section , with the length of 299 km . the section are wide and shallow , the flow state of the section is turbulent with a swing mainflow
黄河下游河南孟津铁谢至山东高村299公里游荡性河段，河道宽浅，河势散乱，主流摇摆不定，是黄河下游河道整治的重点和难点。 - The dissertation focus on the main conflict of flow and sediment change , by analyzing the flow and sediment features , and change in rivercourse of typical period in histry , collecting the data of riverbed change . according to the flow and sediment change condition , combining the existed water works , and based on the results of former researches , the study are conducted on the law of flow state change by comparing rivercourse conditions before and after the completion of sanmenxia project , which may provide some idea for flow state change when xiaolangdi project completed and put into operation and some basic clue for the prediction of variation trend of river section from tiexie to shendi , from shendi to tieqiao near zhengzhou , from tieqiao near zhengzhou to dongbatou , from dongbatou to gaocun and so on in the year 2010 and the period 2010 to 2020 . the result may provide some reference for flood control of these wangdering river sections , and some guidelines for planning of water projects and arrangement of project sequence
本课题紧紧抓住小浪底水库运用后水沙变化这一主要矛盾，通过分析研究以往典型时期的水沙特点和河道演变特点，收集分析河床边界条件变化资料，小浪底水库运用后水沙资料变化，结合现有河道整治工程建设情况，总结前人的研究成果，重点研究三门峡水库运用后下游河道河势变化的规律和特点，探索小浪底水库运用后下游河势变化情况，分析预测游荡性河道铁谢至神堤、神堤至郑州铁桥、郑州铁桥至东坝头、东坝头至高村等各个河段在2010年， 2010年至2020年期间的河势变化趋势，为分析游荡性河段的防洪形势，指导河道整治工程建设的规划和工程安排提供决策参考和依据。 - According to all the sediment peaks of 35 floods observed at each station on the downstream of xiaolangdi , it analyzes the characteristic of delayed sediment peak and establishes a regression equation between sediment peak lag time for each section of xiaolangdi , huayuankou , jiahetan , gaocun , sunkou , aishan and lijin and peak discharge , sediment concentration of the peak , flood propagation velocity and fall velocity of suspended load of the previous station , which can search , make up and extend sediment peak lag time and provide a basis for accurate forecasting on sediment peak travel time of each station on the lower yellow river
根据小浪底下游各站沙峰均滞后于洪峰的35场洪水，对沙峰滞后于洪峰的特性进行了剖析，建立了小浪底、花园口、夹河滩、高村、孙口、艾山、利津各河段沙峰滞后时间与上站洪峰流量、沙峰含沙量、洪水传播速度、悬移质泥沙群体沉速之间的回归方程，可以用来查补延长沙峰滞后时间，为下游各站沙峰传播时间的准确预报提供依据。