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   地 在 农业经济 分类中 的翻译结果: 查询用时:0.461秒
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  land
    Study on the Mechanism of Chinese Rural Land Transfer
    中国农流转机制研究
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    Study on Land Conversion from Rural to Urban Areas and Its Decision-making
    农城市流转及其决策研究
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    Application of the Central Link Formulae of Man—land Relationship in Land Use to Analyse for Population Growth and Food Production of Guyan County
    用人—关系中环公式对固原县人口增长与粮食生产的分析
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    Worries on the Land in China
    “杞人”忧──中国土忧思录
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    The results showed that the basic cultivated farmland (17.59 104 hectares) in the whole city can be divided into 6 grades, among which the IFI (Integrated fertility index) of the cultivated land at the first grade was bigger than 0.85. Its area was 2.07 104 hectares, accounting for 11.8% of total cultivated area.
    结果表明,全市17.60万hm2基本农田耕可分为6级,其中,1级IFI(力综合指数)>0.85,面积为2.07万hm2,占总面积的11.8%;
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  “地”译为未确定词的双语例句
    A Study of the Farmland Institutions in China
    中国农制度研究
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    The Structure of Farmland Property Rights and Agricultural Performance
    农产权结构与农业绩效
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    Farmland Conversion: Equity, Efficiency, and Public Welfare
    农非农化配置:公平、效率与公共福利
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    Economical Evaluation of Utilization Schemes of Steeper Sloping Lands in Yanchang County
    延长县陡坡利用方案的经济评价
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    On Economic Assessment Principle and Method of Farmland Quality
    农质量经济评价原理和方法的探讨
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  land
Our study indicates that the model can be applied to study the interaction between land surface processes and atmospheric boundary layers over various underlying surfaces and their regional climate effects.
      
Regularities of wind-erosion of different land-use types in Yongding River sandy land, Beijing
      
The threshold wind velocity of a number of variables was studied in four different land-use types: farm land, forestland, wild grassland and a flood plain in the Yongding River sandy land in Beijing.
      
The following conclusions were drawn: 1) The order of decreasing threshold of wind speed for sand displacement and surface roughness were forestland, wild grassland, farm land, sparse wild grassland and flood plain.
      
At a height of 0-20 cm, the height increased while the sediment discharge percent of sand flux decreased; there were significant differences in the sand flow formation under different land-use types.
      
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