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黄土高原

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The main magnetic minerals in L1 and S1 are magnetite, maghemite and ilmenite.

这是黄土高原东缘风成沉积物不同于中、西部黄土的特征。

The Loess Plateau is the most tremendous loess landform of the world .

黄土高原是世界最大的黄土地貌。

The eolian loess-paleosol sequences on the Loess Plateau basically record a history of alternation between winter and summer monsoon dominance, which can be seen as a reflection of global climatic cycles in East Asia. So far, spatial and temporal pattern of East Asian summer monsoon has been reconstructed mainly by magnetic susceptibility record.

黄土高原风成堆积的黄土-古土壤序列完整记录了东亚古季风气候的变迁,即冬季风优势期和夏季风优势期相互交替的历史,可视为全球古气候旋回在东亚地区的表现。

As the representative of the northern Loess Plateau gully region, the soil quality under different cultivation length of the orchard in Changwu county was studied. Using partial correlation coefficient to determine the weight, combined with evaluation of membership Sanction to evaluate soil quality levels of the area, the trend of orchard soil quality under different cultivation years was analyzed. The results showed that the IFI values of orchard soil were between 0.22 and 0.70, 27% of them reached the second soil quality standards, 64% reached a third-level soil quality standards, 9% met the fourth standards of soil quality.

以长武北部黄土高原沟壑区为代表,研究了不同果园种植年限下的土壤质量现状,运用偏相关系数法确定权重,结合隶属度函数评价了该地区土壤的综合肥力水平,分析果树种植中土壤质量随着种植年限的变化趋势,结果表明:黄土沟壑区果园土壤IFI值在0.22~0.70,其中有27%达到了2级土壤质量标准,64%达到了3级土壤质量标准,9%达到了4级土壤质量标准。

Lijiaxia landslide is a large rockslide , encountered in Loess Plateau which is famous for lots of loess landslides .

李家下滑坡是大型岩质滑坡,发育在黄土滑坡众多的黄土高原区。

In Project A, grain shortage will not appear in the corrasive region of Loess Plateau on the whole. But in order to achieve an equilibrium of demand and supply, loess hill regions must import grain from the Loess Platform region.

从A方案看,就黄土高原水土流失区整体而言将不会出现粮食短缺;但具体到分区而言,黄土丘陵区必须通过粮食调入才能满足本区需求,而黄土台塬区则有一定盈余。

The Holocene loess-soil sequence on the Chinese Loess Plateau constitutes an excellent record of evolution of soil formation, monsoonal climate, eolian dust accumulation and influence of arable farming of over 10000 years.

黄土高原的全新世黄土-土壤地层系列很好地记录了过去一万多年土壤发育、季风气候、风尘堆积和农业耕作影响的演变。

As an important tectonic boundary of Northeastern Tibetan Plateau, the Liupan Shan is closely influenced by the uplift/growth process of the Tibetan Plateau, it also plays an important role on the paleogeographic evolution of Chinese Loess Plateau.

作为青藏高原的东北构造边界的六盘山,它的形成演化与青藏高原隆升/增生息息相关,同时六盘山的隆升对黄土高原古地理分异演化产生了重大影响。

Hilly gullied loess region, the main body of Loess Plateau, is also an eco-economic sensitive area with special landscape pattern.

黄土丘陵沟壑区是黄土高原的主体部分,也是具有特殊景观格局的生态-经济敏感区。

To construct large rainwater collecting and storing projects in line with local conditions in gullied rolling loess area of the Loess Plateau can effectively utilize the rainwater resources and provide services for soil and water conservation measures and production and life of the local people.

黄土高原的黄土丘陵沟壑区因地制宜建设大型雨水集蓄工程,可有效利用雨水资源,为水保措施和当地群众的生产生活服务。

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