Loess Plateau是什么意思_Loess Plateau的中文翻译|音标|读音|用法|短语例句|近反义词

1、

Spatial and Temporal Characteristics of Air Temperature in China Loess Plateau in Spring

中国黄土高原地区春季气温时空特征分析

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2、

Influence of Soil Moisture on Exchange between Water and Gas of Oriental Arborvitae at Semi-Arid Region of Loess Plateau

黄土半干旱区土壤水分对侧柏叶片水气交换影响

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3、

Desiccation of deep soil layer and soil water cycle characteristics on the Loess Plateau

黄土区深层土壤干燥化与土壤水分循环特征

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4、

The vegetation restoration and construction the Loess Plateau is a key ecological engineering in Chi-na.

黄土高原地区植被恢复与建设是我国重大的生态工程,有巨大的战略意义.

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5、

Aboveground productivity and soil water characteristics of cultivated Old World bluestem grassland in semi-arid loess hilly-gully areas on the Loess Plateau

半干旱黄土丘陵区白羊草人工草地生产力和土壤水分特征研究

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6、

Shaanbei Luochuan loess plateau is one of soil erosion districts slump.

陕北洛川黄土塬是水土流失严重的地区.

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7、

Prehistoric Vegetation on the Loess Plateau: Steppe or Forest?

史前黄土高原的自然植被景观──森林还是草原?

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8、

Preliminary Research on Countermeasures of Desiccation of Deep Soil Layer in Loess Plateau

黄土高原土壤干层减缓方法初探

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9、

High soil erosion rate by water mainly relates to low soil anti-scouribility in the Loess Plateau.

在水土流失极为严重的黄土高原地区,土壤抗冲性决定着土壤的可蚀性.

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10、

Water Physiological Ecology Characteristics and Community Biomass of Lespedeza davurica under Different Habitats in Gully Areas of Loess Plateau

黄土丘陵区不同立地达乌里胡枝子群落水分特征及生物量研究

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11、

Irrigated farming is the primary kind of agricultures in loess plateau.

黄土高原自然条件特殊,耕作农业以引水灌溉为主.

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12、

Achnatherum splendens , belongs to the grass family, largely distributes in Loess Plateau.

芨芨草是黄土高原地区广泛分布的禾本科植物.

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13、

Study on the Management Database of Land Resources at Xixian Broken Loess Plateau Region

隰县试区土地资源管理数据库的建立与运行

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14、

Characteristics of Soil Aridity in Wheat Field of the Longdong Loess Plateau

黄土高原塬区麦田土壤干旱特征

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15、

Hilly-gullies Loess region is the most fragile and underdeveloped area of the Loess Plateau.

黄土丘陵沟壑区是黄土高原生态环境极其脆弱,经济发展十分落后的地区.

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16、

Dingxi Prefecture is located in the foothill of the Loess Plateau climate is arid or semi-arid.

位于黄土高原丘陵沟壑干旱半干旱区的甘肃省定西地区,面临生态恶劣和经济贫困的双重危机.

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17、

Hunyuan County is located in the Loess Plateau area on the edge, complex landform, diversified structure.

浑源县地处黄土高原的边缘地带, 地貌类型复杂, 结构多样.

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18、

The scope, geographic location, climatic features of Loess Plateau and its shelter forest are introduced here.

简述了我国黄土高原的范围、地理位置、自然气候特征及防护林建设成就.

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19、

A Study on Mathematical Model of Chinese Arborvitae Leaf Transpiration in the Semi-arid Region of the Loess Plateau

半干旱黄土地区幼龄侧柏叶蒸腾的数学模型

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20、

Coal field seismic prospecting in loess plateau or complicated loess topographic area needs going on the research of crook seismic working technology along channel.

在黄土塬区或复杂的黄土地形区作煤田地震勘探工作需要进行沿沟弯线地震施工技术的研究。

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21、

The study was in acoal mining industrial area Honggu coal mining in Lanzhou, Loess Plateau.

以黄土高原兰州红古矿区为例,研究煤矸石长期堆积对当地土壤产生的重金属污染.

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22、

Township iscan yuan gully region of Loess Plateau.

全乡属黄土高原残垣沟壑区.

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23、

There are several intermittent streams in the Loess Plateau.

在黄土高坡上有数条干涸的间歇河.

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24、

Result of the analysis indicates low diversity which implies highly fragmented situation of soil landscape pattern in Loess Plateau.

结果表明，黄土高原地区土壤景观斑块数、面积和周长分布均极不均衡，土壤景观多样性指数较低，反映出黄土高原地区土壤景观破碎化程度较高。

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25、

Paleomonsoon evolution and Heinrich events: evidence from the Loess Plateau and the South China Sea

黄土高原和南海陆架古季风演变的生物记录与Heinrich事件

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26、

Neotectonics was the dominant factor of the environmental evolution of Loess Plateau.

新构造运动是黄土高原区域环境变迁的主导性因素.

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27、

As underground water buried deeply in Loess Plateau, the soil water from precipitation influx is the main source to the vegetation. The volume of soil water decides the kind of vegetation in the area.

在黄土高原地区，由于地下水埋深大，该区植被的发育主要依靠来自大气降水入渗形成的土壤水分，所以土壤水分的多少是决定不同类型植被发育的最关键因素。

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28、

Study on Establishing Soil Landscape Ecology Information System in Loess Plateau by GIS

GIS支持下的黄土高原土壤景观生态信息系统研究

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29、

Eastping xiang combination is located in the Qinghai-Tibet Plateau and the Loess Plateau area.

东坪乡地处青藏高原与黄土高原结合地带.

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30、

Yang W Z, Shao M A. Study on Soil Moisture in Loess Plateau.

杨文治, 邵明安. 黄土高原土壤水分研究.北京:科学出版社,2000,10:174-177.

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