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   desert 在 自然地理学和测绘学 分类中 的翻译结果:
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      desert
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  沙漠
    Water and Salt Movement in Soil of Takelamakan Desert Irrigated with Saline Water
    咸水灌溉条件下塔克拉玛干沙漠土壤的水盐运移规律
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    Changes of Surface Feature of the stablized Mobile Dunes at shaqotous Southeast Egqe ofTengger Desert
    腾格里沙漠东南缘沙坡头地区流沙治理后地表形态的变化
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    Study on Formation and Development of Aeolian Landform and Trend of Environmental Change at Lower Reach of the Keriya River, Taklimakan Desert
    塔克拉玛干沙漠克里雅河下游地区风沙地貌的形成发育与环境变化趋势的初步研究
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    Historical Geography Study of the Hobq Desert
    库布齐沙漠历史地理研究
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    The Environmental Significance of Vegetation Cones of the Taklimakan Desert,China
    塔克拉玛干沙漠灌草丘的发育特征及环境意义
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  荒漠
    PROBLEMS ON THE DISTRIBUTION AND CLASSIFICATION OF DESERT SOILSIN WESTERN TIBETAN PLATEAU, CHINA
    西藏高原西部荒漠土壤分布与分类问题——兼与有关人士商榷
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    Tamarix spp.── The Keyston Species of Desert Ecosystem
    中亚荒漠生态系统中的关键种──柽柳(Tamarixspp.)
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    Strategic Measures for Sustainable Agricultural Development in Desert Regions
    荒漠碱化土区域农业持续发展战略
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    Analysis of Inverse Humidity and Moisture Respiration Process of Surface Soil in Desert Near Oasis
    邻近绿洲的荒漠表层土壤逆湿和对水分"呼吸"过程的分析
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    Characteristic Analysis on the Mountain,Oasis and Desert System
    山地、绿洲、荒漠系统的特征分析
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  沙漠的
    The Formation of Proglacial Desert on the West of Icefield Puruogangri and Discovery of Glacial-Type Desert in China
    普若岗日冰原西侧冰前风沙地貌的形成与我国冰川型沙漠的发现
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    Discussion on desert formation from viewpoint of coupling of the earth and atmosphere
    从地气耦合角度讨论沙漠的成因
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    Study on Takelimgan Desert Using ShenZhou-IV Spaceborne Multiple Band Microwave Radiometer
    利用神舟4号飞船多频段微波辐射计对塔克拉玛干沙漠的研究
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    Till the late stage of the desert, the divergent latitudes was drifted southwards due to the lond period climatic fluctuations and thus the whole desert was within the extent of the westerly winds.
    该沙漠的晚期,由于气候的长周期波动,切变带南移,整个沙漠完全被西风带控制。
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    The formation of the plateau created sandy substance and accelerated the formation of south-east monsoon system and other climate changes, which directly influenced the occurring of desert in geologic period, and indirectly influenced the desertification of North China in the historic period by effecting the early living pattern of man.
    青藏高原的隆起为中国沙漠与沙漠化的形成创造了丰富的沙地基质 ,促进了我国东南季风的形成及其他相应的气候变化 ,气候的变化直接的影响了我国地质时期沙漠的形成 ,并且通过影响我国北方早期人类活动的集聚格局间接影响了我国历史时期沙漠化的发展。
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  “desert”译为未确定词的双语例句
    Design and Compilation Of Aeolian Landf orm Map Of Badain Jaran Desert
    巴丹吉林风沙地貌图设计与编制
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    Study on Soil Element Background Values of the Taklamakan Desert
    塔克拉玛干沙漠地区土壤元素背景值研究
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    5. 9% and4. 2%. (2) Ca2-P was the main resource pf the quick-acting phosphor of the Grey desert soil.
    (2)Ca2-P是灰漠土中主要的速效磷来源,其次是Al-P和Fe—P;
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    The A1-P and Fe-P were the second resource. The Ca10-P and Ca8-P were the phosphor depository of the Grey desert soil promoting the transform from the CalO-P and Ca8-P to the Ca2-P was the key factor pf raising the supplying phosphor capability of the Grey desert soil.
    Ca10—P和Ca8-P是灰漠土的磷库,如何促进Ca10-P和Ca8-P向Ca2-P转化是提高灰漠土供磷能力的关键因素。
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    The principal component analysis of salinized situation in desert land of Chaidamu basin
    柴达木盆地弃耕地盐渍状况的主分量分析
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  desert
       Experimental Studies on the Natural Restoration and the Artificial Culture of the Moss Crusts on Fixed Dunes in the Tengger Desert, China
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       Bryum argenteum is the dominant species of moss crusts in the Shapotou region (104°57'E, 37°27'N) of the Tengger Desert.
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       The highest species richness and aboveground productivity were found in alpine meadow, followed by meadow steppe, typical steppe and desert steppe.
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       Niche characteristics of rodents by diverse disturbance in Alashan desert, Inner Mongolia, China
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       Four diverse disturbance types, namely, farmland, rotationally grazed grassland, overgrazed grassland and forbidden grazing grassland, were identified in the Alashan desert region of Inner Mongolia.
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         The research in the Loess Plateau of China, has had a very long history. The changes of the natural environment are very obvious and the effects on-the neighbouring North China Plain have been great. Since the founding of the people's Republic of China, alor with the vigorous development of our national economy, science and culturt, the historical-geographical scholars of China have studied the loess Plateau from many aspects and have gained great success. Progress in research work, on the whole, may be div...
            本文将建国以来我国黄土高原历史地理研究工作划分成五十年代至六十年代前期、七十年代后期迄今两个阶段,从历史时期气候变迁、农牧业发展及分布区域的变化、土地利用方式与黄河下游安危的关系、植被变迁、黄土侵蚀地貌成因、河湖水系变化、沙漠变迁等七个方面介绍了所取得的主要研究成果及其意义,对今后如何进一步开展这一领域的研究工作提出了意见。
文摘来源
         The study of the formation mechanism of aeolian landform hasn't been made new progress in recent years, and at present it is a key aspect on the research, theoretically and practically, of desert science. On the basis of field observation, many scientists in the field in various countries have proposed some hypotheses, but nowaday these hypotheses are still being under exploration and not identified by site-observations, and at the same time, its physical process is lack of clear delineation.
            本文以新月形沙丘为例,分析了风沙运动物理过程,说明风沙地貌的发生和发展情况。作者认为,风沙有自动聚集成堆的收敛性,而沙粒一旦成堆,下层的沙粒将受到保护成为不可动粒子。另一方面,沙粒成堆后运动将变慢,上风的风沙流不断补充,致使沙堆逐渐增大而发育为典型的风沙地貌。
文摘来源
         This paper mainly states the surface micro-structure shape of China's arenaceous quartz, which is formed under the effect of external building force as glacier, water flow ( including rivers, morning and evening tides ) and wind erosion etc. According to this, the evolution history of sandy deposites and the relationship between the shape structure of sandy material and the cause of formation can be further investigated offer grounds of argument on source of sandy material in desert.
            本文着重论述了我国石英砂粒在冰川、水流(包括河流及潮汐)、风蚀等外营力作用下,形成的特有微结构颗粒表面的形态。据此,探索沙质沉积物的演变历史,沙物质形态结构与成因的关系,为沙漠沙物质来源提供论据。
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