1)North China Plain华北平原
1.Life Cycle Environmental Impact Assessment of Winter Wheat in North China Plain;华北平原冬小麦生命周期环境影响评价
2.Validation of the Feasibility of MOD16 Algorithm for Estimating Crop Field Vapor Flux in North China Plain;MODIS水汽通量估算方法在华北平原农田的适应性验证
3.Exploring an Ecological Benefit of South - to - North Water Transfers for Rehabilitating Groundwater Systems in The North China Plain;发挥南水北调的生态效益 修复华北平原地下水
英文短句/例句
1.Experimental Study on Practical Agricultural Water-saving Measures on Huabei Plain;华北平原农业节水实用措施试验研究
2.Studyon Sustainable Utilization of Groundwater in North China Plain华北平原地下水资源可持续利用研究
3.Study on the Features of the UV-B Radiation and Ecological Effects in North China Plain;华北平原北部太阳辐射特征及生态效应研究
4.Research on Groundwater Regulation and Recoveryin North China Plain after the Implementation of South-to-North Water Transfer南水北调实施后华北平原地下水调控研究
5.THE DISTRIBUTION AND RECLAMATION OF SALINE-ALKALI SOILS OF NORTH CHINA PLAIN AND THE WEI-HO PLAIN IN THE PERIOD OF CHOU-HAN DYNASTIES周秦两汉时代华北平原与渭河平原盐碱土的分布及利用改良
6.Conditional Simulation of Hydro-geological Structure and Its Application in Plain Area:A Case Study of North China Plain平原地区水文地质结构条件模拟及其应用:以华北平原为例
7.THE APPLICABILITY RESEARCH OF WOFOST MODEL IN NORTH CHINA PLAIN作物生长模型WOFOST在华北平原的适用性研究
8.DEVELOPMENT AND GEOGRAPHICAL DISTRIBUTION OF THE COLONY OF TOWN NAMES IN THE NORTH CHINA PLAIN华北平原城镇地名群的发展及其地理分布特征
9.Taihang Mountain, standing on the edge of Campagna of North-China, is the headstream of Hai River.太行山雄居华北平原西缘，是海河的发源地。
10.Study on the Restrictive Factors for Bird Survival in Cultivation Areas of North China Plain华北平原耕作区鸟类生存制约因子初步研究
11.Methane Fluxes and the Influential Factors in the Typical Farmlands in the North China Plain;华北平原典型农田甲烷通量及其影响因子研究
12.Ammonia Volatilization from Nitrogen Fertilization in Winter Wheat-Summer Maize Rotation System in the North China Plain;华北平原冬小麦—夏玉米轮作体系氮肥的氨挥发
13.Energy Efficiency of Fertilization in the Production of Wheat and Maize in the Northern China Plain;华北平原小麦和玉米生产中施肥的能量效率
14.Groundwater Age and Recharge Temperature in the Quantenary Aquifers in North China Plain;华北平原第四系含水层地下水年龄与补给温度
15.Research on Evolvement of Shallow Groundwater System Impacted by Exploiting in North China Plain;开采条件下华北平原浅层地下水系统演变研究
16.The Study on Water Consumption Characteristics of Poplar Sheltbelts System in the Cropland of North China Plain;华北平原杨树农田防护林系统耗水特征的研究
17.The Growth Process and Influencing Factors of Villages in North China Plain of Ming-Qing Period;人口的增殖流动与明清华北平原的村落发展
18.The Subdivision and Concentration of Villages in Huabei Plain in the Ming and Qing Dynasties;明清华北平原村落的裂变分化与密集化过程
相关短句/例句
The North China Plain华北平原
1.Lithostratigraphy,Biostratigraphy and Climatic Stratigraphy in the North China Plain since Late Pleistocene华北平原晚更新世以来岩石地层、生物地层及气候地层
2.Published data in literatures were used to estimate the effect of crop residue amendment on carbon sequestration in agriculture in the North China Plain.根据公开发表的文献资料中的数据,从秸秆还田对土壤有机碳的增加、对生物量碳的增加和秸秆还田减少化学N、P、K肥料的使用可减排碳三个方面,定量研究了华北平原冬小麦-玉米轮作区秸秆还田对农田生态系统碳截留的作用。
3.This study investigated variations in soil respiration under different cultivation practices on high yield farmland in the North China Plain during 2004.对华北平原高产农田生态系统2004年的土壤呼吸状况进行了分析,探讨了不同耕作方式下土壤呼吸量的季节变化规律。
3)North China plain area华北平原区
1.In combination with the specific geographic characteristics of Daguang Expressway Shenzhou-Daming section,the author puts forward a design idea for the use of seepage well on expressways intersected with under-pass highways in the light of general highness of subgrade on North China plain area.针对华北平原区路基高度普遍偏高以及河北省大广高速公路深州至大名段的地质特点,提出渗井在高速公路下穿式被交道路中的设计思路,并结合具体应用分析其带来的经济效益,对于实现公路建设的可持续发展和"环境友好"、"资源节约"的环保型公路建设的目的,具有积极的促进作用。
4)Alluvial plain of north China华北冲积平原
5)North China seismic belt华北平原地震带
6)North China Plain region华北平原地区
延伸阅读
华北平原华北平原中国第二大平原。位于黄河下游。西起太行山脉和豫西山地，东到黄海、渤海和山东丘陵，北起燕山山脉，西南到桐柏山和大别山，东南至苏、皖北部，与长江中下游平原相连。延展在北京市、天津市、河北省、山东省、河南省、安徽省和江苏省等7省、市的境域。面积约30万平方千米。主要由黄河、淮河、海河、滦河冲积而成，故又称黄淮海平原。黄河下游天然地横贯中部，分南北两部分：南面为黄淮平原，北面为海河平原。近百年来，黄河在这里填海造陆面积2300平方千米。平原还不断地向海洋延伸，最迅速的是黄河三角洲地区，平均每年2～3千米。地势低平，大部分海拔50米以下，东部沿海平原海拔10米以下。自西向东微斜。主要属于新生代的巨大坳陷，沉积厚度1500～5000米左右。平原多低洼地、湖沼。集中分布在黄河冲积扇北面保定与天津大沽之间。冲积扇东缘与山东丘陵接触处，排水不畅，地下水位高，易受洪水内涝威胁，形成盐碱地。1949年后进行了改造治理。属暖温带大陆性气候，四季变化明显。南部淮河流域处于向亚热带过渡地区，其气温和降水量都比北部高。平原年均温8～15℃，冬季寒冷干燥，最冷月（1月）均温0～－6℃，夏季高温多雨最热月（7月）均温28℃，年均降水量为600～800毫米；无霜期6～8个月；日照充分，大部分全年平均日照时数2300～2800小时，农作物大多为两年三熟，南部一年两熟。土层深厚，土质肥沃。主要粮食作物有小麦、水稻、玉米、高粱、谷子和甘薯等，经济作物主要有棉花、花生、芝麻、大豆和烟草等。矿产资源丰富，有煤、石油、铁矿等，有中国著名的大港油田和胜利油田。东部渤海、黄海沿岸，地面平坦，宜晒海盐，有著名的长芦盐区和苏北盐区，以及重要的盐碱工业基地。华北平原是中国古代文化的摇篮，有许多古老城市，如北京（蓟）、邯郸、开封、商丘、淮阳等。
