区域分异的英文

• regional differentiation

• "区域"英文翻译    area; beat; reach; domain; p ...
• "分"英文翻译    component
• "异"英文翻译    different
• "地域分异" 英文翻译 :    areal differentiation; arealdifferentiation
• "区域分析 区域分析" 英文翻译 :    regional analysis
• "按区域分割" 英文翻译 :    region dependent segmentation; region-dependent segmentation
• "古区域分布" 英文翻译 :    palaeoareal
• "区域分包" 英文翻译 :    regional subcontracting
• "区域分布" 英文翻译 :    area distribution; areal distribution
• "区域分部" 英文翻译 :    georgraphical departmentalization; territorial departmentalization
• "区域分带" 英文翻译 :    regional zoning
• "区域分割" 英文翻译 :    region segmentation; region-dependent segmentation
• "区域分隔带" 英文翻译 :    area separator
• "区域分工" 英文翻译 :    regionale arbeitsteilung
• "区域分化" 英文翻译 :    individuation; regional differentiation
• "区域分级" 英文翻译 :    area classification; local gradation
• "区域分解" 英文翻译 :    domain decomposition
• "区域分界" 英文翻译 :    area limit
• "区域分类" 英文翻译 :    territorial classification
• "区域分配" 英文翻译 :    zone allocation
• "区域分配图" 英文翻译 :    area allocation diagram
• "区域分析" 英文翻译 :    regional analysis
• "区域分销商" 英文翻译 :    regional distributor
• "区域分组" 英文翻译 :    territorial classification
• "关键区域分析" 英文翻译 :    critical area analysis

• Regional variation features of sediment yield intensity in the wei river basin
  渭河流域侵蚀产沙强度的区域分异特征
• City soil and water loss ; water loss ; tri - dimensional system ; region different characters
  城市水土流失水资源流失立体系统区域分异特征
• On dynamics and causes of the regional differentiation characteristics of the foreign direct investment in the united states
  美国外商直接投资区域分异动态变化与成因
• The spatial heterogeneity of climate and precipitation and the water resources in the loess plateau area are analyzed and discussed
  对黄土高原地区气候?降水的区域分异及水资源状况进行了分析。
• The study carries out comparative analysis of change of land use structure of main urban areas and various counties ( cities ) of chuzhou to find out the regional differentiation characteristics of change of land use structure
  对滁州市主城区和各县（市）的土地利用结构变化进行比较分析，以得出土地利用结构变化的区域分异特征。
• Firstly , the author analyzes the scale alteration of towns in county administrative areas from the whole and different parts . this chapter points out two things : on the one hand , the difference between centre - towns and general - towns become more and more prominent , especially county town
  作者首先分析江苏省县域城镇规模变动的过程和现状特点，指出等级分化日益显著，县城镇超前发展，建制镇增长过快，乡镇规模过小及区域分异明显等客观事实。
• Meanwhile , most aspects about this perspective are concerned , which include quantification of the soil water background of the plateau area , the regional spatial variation of soil water background and variation along the slope , mosaic structure and seasonal changes etc . the results show that : ( 1 ) for the fundamental circumstance for vegetation development is the original debilitated slope , so the perspective of soil water background specially for the loess plateau refers to the soil water conditions on the original slope . ( 2 ) the value of soil water background appears to be a descending trend from south to north based on the difference of vegetation zones . in the forest zone , soil moisture contents beneath 3m depth from the soil surface are more than 12 % usually ; in the forest - pasture zone , the values of soil moisture content beneath 4m depth underground are more than 6 % and stable , and tend to be ascending while the depth increases ; but the values in the dry pasture zone is lingering between 4 % to 6 % from the surface layer to sub - layers
  发展了“土壤水分背景”的概念，并以之为基础对其各个方面进行了研究，使之形成一个相对独立和完整的体系，主要包括黄土高原土壤水分的背景值、土壤水分背景的区域分异、坡面分异、镶嵌结构及其季节分异等： ( 1 )由于植被生长发展、演替的基础阶段是天然草被群落，故认为黄土高原的土壤水分背景在概念上是特指该区天然草被群落下的土壤水分状况； ( 2 )黄土高原的土壤水分背景值，根据植被地带的不同表现出自南向北逐渐降低的规律：森林地带3米以下土层水分背景值普遍稳定地高于12 ，森林草原地带4米以下土层水分背景值稳定大于6 ，且均随土层的加深水分含量逐渐增加，而草原带的土壤水分背景值自土表至底土层一直在4 6之间徘徊。
• First , according to the heterogeneity of landscape in zherong , the author selected the dominant elements such as topography , altitude and climate which reflect the large scale of area differences and the stastistical materials which have long - reaching effects on the county . the county was divided into 8 landscape types : resident and trade area , industry area , traffic land , farmland , garden and greening land , water area , forestry area , unclaimed land . the types have 21 subtypes , the city area , county area , heavily polluted industry area , little maching area , road land , country road land , cultivated land . mushroom land . taizishen land , tea land , man - made greening land , garden land , reservoir area , river and creek area . defending forestry area , forbid - cut forestry area , bamboo area , economical forestry area , unclaimed mountain , unclaimed land , unclaimed water
  同时，根据该县景观异质性强的特点，以行政区划单位、人为干扰强度、景观要素和功能流为柘荣县城市景观分类的原则和依据，选择地貌、海拔、气候等反映区域分异的主导因子和对该县社会经济影响深远的统计资料，将全县划分为8个景观类型，即居住区和商业区景观、工业区景观、交通用地景观、农田景观、公园绿地景观、水体景观、林区景观、未开发地景观。景观类型下又划分21景观亚类型，分别为城区景观、村落聚居地景观、重污染工业景观、小加工业景观、公路景观、乡村道路景观、耕地景观、食用菌景观、太子参景观、茶园景观、人造绿地景观、公园景观、水库景观、溪河景观、防护林景观、封山育林区景观、竹林景观、经济林景观、荒山景观、荒水景观、荒地景观等景观亚类型。
• The dry / wet changes of surrounding area of bohai sea during past 500 years are divided into 7 stages , based on dry / wet indexes ( d / w ) of this area from 1470 to 1985 then , the changes of dry / wet spatial types ( d / wst ) and its related dry / wet regional different iation ( d / wrd ) features among different stages are analyzed . the results show that there are 4 main kinds of d / wst in this area , whose notability and spatial distribution features in different stages are apparently different , which reflects , very well , the changing process of the d / wrd of this region in past500 years . further analysis also presents that , in warmer period , the d / wst and the d / wrd patterns are relatively unsteady , meanwhile , the dry / wet changing difference among different parts of the region is relatively great , but , in colder period , it is just on the contrary . however , in the most severely cold period of the little ice age , t he area ' s d / wst and the d / wrd pattern sareveryu nsteady , and its d / wrd extenti salsot he high estin the whole past 500 years
  用研究区1470 1985年的旱涝等级资料,划分了该地区500年来旱涝变化的7个阶段,讨论了不同阶段间旱涝型的变化及其旱涝区域分异意义,结果表明, 500年来研究区有4类主要旱涝型,各型旱涝在不同阶段的重要程度及场型特征均有较大差异,深刻反映了该地区500年来旱涝区域分异特征的变化,通过对500年来旱涝变化与温度变化的对比发现,较温暖期,研究区的旱涝型及旱涝区域分异格局较多变,旱涝变化的区域差异性较大,较寒冷期,旱涝型及区域分异格局较稳定,旱涝变化的区域差异性较小,而在小冰期最寒冷阶段,旱涝型及旱涝区域分异格局的变动十分频繁,旱涝变化的区域差异性亦最大