和田河

  • 网络Hotan River;Khotan-daria
和田河和田河
  1. 和田河流域水资源保护规划研究

    Study on Water Resources Protection Planning of Hotan River Basin

  2. 和田河流域土地利用变化及其生态环境效应分析

    Analysis on Land Use Changes and Their Ecological Effect in Hotan River Basin

  3. 烃类组分、非烃组分分布以及天然气δ~(13)C1值在和田河气田的东、西部存在明显的差异。

    The content of hydrocarbon and non-hydrocarbon gases and δ 13C1 values in the eastern part of the field are obviously different from those in the western part .

  4. 和田河流域生态脆弱性成因辨识

    The reason for ecological fragility in Hotan river basin

  5. 气候变化对和田河夏季平均流量的影响

    Analysis on the Influence of Climate Change on Aestival Runoff Volume of the Hotan River

  6. 和田河偏少17.9%,为枯水年。

    Hotan River , decreasing by 17.9 % , was a shortage of water year .

  7. 和田河流域中游生态系统健康评价的框架构建

    Framework Establishment of Ecosystem Health Assessment in Middle Reaches of Hotan River Watershed , Xinjiang

  8. 塔里木盆地和田河气田的天然气具备水溶气成藏地球化学特征和理想的水溶气成藏条件。

    The Hetianhe gas field of Tarim Basin has excellent geological conditions for water-soluble gas accumulation .

  9. 水文要素对人类活动响应的研究&以和田河流域为例

    Research on the Responses of the Hydrological Factors to Human Activities & Case Study of Hotan River Basin

  10. 新疆和田河流域土地利用及其生态服务价值变化

    Study on Land Use Change and Its Effect on Ecological Service Value in the Hotan River Basin , Xinjiang

  11. 长江上游干流区径流变化规律及预测研究新疆和田河流域河川径流时序特征分析

    Upper Yangtze River Annual Runoff Analysis and Its Forecast Analysis on the Characteristics of Annual Runoff in Hotan Catchment

  12. 塔里木盆地和田河气田天然气的特殊来源及非烃组分的成因

    Special Source of the Natural Gases of the Hotan River Gas Field and the Origin of Its Non-Hydrocarbon Gases

  13. 和田河气田天然气以烃类气体为主,但含有较高的非烃气体,含量一般为10%~25%。

    The gases are mainly composed of hydrocarbon components , with higher non-hydrocarbon components from 10 % to 25 % .

  14. 新疆和田河流域河川径流混沌特性分析卡盖拉河流域管理开发组织

    Chaotic characteristics of annual runoff in Hotan Catchment ; Organization for the Management and Development of the Kagara River Basin

  15. 和田河流域脆弱生态环境是水、植被环境恶化导致的生态平衡失调形成的。

    Both water and vegetation environment worsening caused ecological imbalance , which caused the fragile ecological environment in Hotan river basin .

  16. 水是和田河绿色走廊形成与演变最重要的因素。

    The water resources is the most important factor in the formation and evolution of the green corridor of Hetian River .

  17. 和田河流域径流过程的研究对于维持绿洲内的水土资源平衡、合理利用流域内有限水资源具有重要的现实意义。

    Researches on runoff process are beneficial for the sustainable utilization of water resources , water conservancy planning and the development of agriculture .

  18. 和田河气田是塔里木油田分公司“九五”期间探明的大型气田。

    Hetianhe gas field , a large scale carbonate gas pool proved by Branch Company of Tarim Oilfield during the ninth five year plan .

  19. 和田河是目前唯一穿越塔克拉玛干沙漠的河流,和田河地表水资源是和田绿洲的主要水源,浇灌着塔克拉玛干沙漠中的绿色走廊。

    As the only river that traverses the Taklimakan Desert , water resources in Hotan Catchment is the main source of Hotan oasis-Green Corridor in the Desert .

  20. 经过对和田河流域森林生态系统定量评价、分析、研究得出以下主要成果:(1)和田河森林生态系统服务价值总值是2960.62-2963.19亿元/a。

    After rational evaluating , the author put the main fruits as following : The total ecological service value of the forest ecological system in Khotan drainage basin is 296.062-296.319 billion Yuan annually .

  21. 在对和田河开发、利用及保护现状调查的基础上,根据《全国水功能区划技术大纲》对和田河进行了水功能区划;

    Based on analyzing the present situation of exploitation , utilization and protection of Hotan river , according national technical outline of water function regionalization , divided the water function of Hotan river .

  22. 本论文以和田河流域为例,对遥感方法在西北干旱地区绿洲生态地质环境评价中的应用进行了探讨。

    In this thesis , it is concerned with that the remote sensing method is applied to the evaluation of ecological geological environment , as an example , on the inland river basin in the arid northwest China .

  23. 和田河是和田绿洲农业灌溉的主要水源,对于和田绿洲的人民生活、工农业生产,对于阻止沙漠进逼、维持绿洲的稳定具有重要的意义。

    Hotan river is the main water resources of agricultural irrigation in Hotan oasis . It has very important significance for people living , industrial and agricultural production in Hotan oasis and to prevent the approach of desert , maintain the stabilization of oasis .

  24. 和田河属融水型洪水,量大峰缓,两支流易同时遭遇大洪水,洪水系列具有3.8年和11年的周期;

    The floods occur mainly because the glacier and snow melt , whose total quantity are very large and flood peak are relative flat . The high floods often happen simultaneously on the two tributaries and the series of flood has the period of 3.8 and 11 years .

  25. 结果表明:近44a来和田河流域夏季高空500~300hPa平均气温和0℃层高度呈下降趋势,倾向率分别为-0.322℃/10a、-32.42gpm/10a;夏季流量也呈下降趋势,其倾向率为-7.26m3s-1/10a。

    The results are shown the average temperature between 500 hPa and 300 hPa , 0 ℃ level height and the aestival runoff volume decrease at the rate of - 0.322 ℃ / 10a , -32.42 gpm / 10a and -7.26 m3s-1 / 10a respectively in the recent 44 years .

  26. 本文主要分析和模拟了和田河流域的径流过程,大致分为三个部分:径流时间序列分析、源流山区降雨径流模拟和平原区河道洪水演进。

    The paper is composed of three parts , analysis of runoff process , source area rainfall runoff simulation and flood channel routing in plain .