镶嵌结构 meaning in English
mosaic structure
mosaic texture
mosaictexture
pattern structure
Examples
- Fractal model study on mosaic structure of dongting lake area
洞庭湖区景观镶嵌结构和分形特征研究 - Mosaic structure and heating treatment of passivated hgcdte
钝化过程中形成的镶嵌结构及其热处理效应 - The gis technique supported by arc / info software was used to analyze the heterogeneity of oasis - desert ecosystem and its mosaic of patch structure , landscape change in fukang transect
利用地理信息系统软件对阜康绿洲-荒漠生态系统的景观结构的异质性、镶嵌结构及其格局变化进行了较全面的分析。 - 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。 - ( 2 ) parts of the area show apparent local climatic properties because of the influence of topography , landcover , and so on . precipitation in mountainous and forest area is usually more affluent than in vicinity , this creates a typical mosaic structure of precipitation distribution like the islands . ( 3 ) soil water is the most significant form of water resources , which is the only water for vegetation uptake
分析结果显示： ( 1 )黄土高原地区的降水分布自东向西、自南向北逐渐减少，东南部可达900多毫米，西北部最低则仅约100毫米，表现出显著的大陆性气候特征； ( 2 )由于地形等因素的影响，山地森林等局部地区小气候特征明显，降水量高于周围地区，结果形成降水的岛状镶嵌结构； ( 3 )土壤水是黄土高原最重要的水资源之一，它是该区植被水分利用的重要资源。