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艾比湖的英文

音标：[ àibǐhú ]  发音:  
"艾比湖"怎么读用"艾比湖"造句

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  • ebinur hu

例句与用法

  • The soil texture determination and analysis in the ebinur lake area
    艾比湖湖区土壤质地测定及其分析
  • Contemporary aspect of wetland protection and environmental improvement in the abi lake area
    保护湿地改善艾比湖流域生态环境
  • After the investigation , the river in kuitun has not the surface water going into ebinur from 70 ' s to now
    经访问调查,奎屯河于70年代末,已无地表水进入艾比湖。
  • Therefore , the general trend of ebinur lake ’ s development in the future is in water shortage . in some special periods , the annual and age lake area sometime will exceed 800km2 1000km2 . but the frequency is not high , it will have less effect on the
    因此,艾比湖未来发展总体趋势仍处于缺水状况,在年内和年际某些特殊时段,湖面会出现超过800km2 1000km2的短时过程,但出现的频次不高,对沿湖铁路线的影响较小。
  • This paper studies ebinur lake area in annual and age scales , finds out there are remarkable annual and age changes . based on the analysis of causes of ebinur lake area dynamic changes , the research concludes that the lake area change generally falls into two phases
    本文从年内与年际尺度对艾比湖湖面变化进行研究,发现湖面年内年际变化都很显著,在剖析湖面动态变化原因的基础上,得出近50年来艾比湖湖面变化大体上可分为两个阶段。
  • This paper systematically analyzes the environmental effect of the ebinur lake area dynamic change and its influence on the railway along the lake , and the research establishes water balance equation of the ebinur lake , chooses the two characteristic phases , 1991 1992 , 1998 1999 , for computing , and concludes that since 1990s , water storage whether in low water period or in high water period is less than that of 1960s , whose lake area was 800km2 , and this area basically can reach the target of optimal eco - environment benefit
    本文系统地分析了艾比湖湖面动态变化的生态环境效应及其对沿湖铁路线的影响。并通过艾比湖水量平衡方程式的建立,选择1991 1992年(枯水时段) 、 1998 1999年(丰水时段)两个特征时段进行计算分析,得出20世纪90年代以来,不论是枯水时段储水量,还是丰水时段储水量,均小于20世纪60年代湖泊水面保持800km2所需水量,而此水面基本可以达到湖区生态环境效益最佳的目标。
  • It lies between the ala mountain pass and the mutataer desert , can regulate climate , defend strong wind , reduce sand - storm and maintain species variety etc . the amount of water flowing into the ebinur lake decreased 23 108m3 ? a - 1 from early 1950 ' s to current along with the rapid increase of population and economy in the valley
    随着1950年代以来,艾比湖流域人口、经济的快速增长,生产、生活用水的成倍增加,汇入艾比湖的水量由建国初期的30 108m3减少至目前的7 108m3左右,湖面也由1200km2干缩到750km2左右。
  • Phase i : 1950s 1980s . in this phase , humans ’ limited cognition of nature laws , increasing demands caused by population explosion and unreasonable utilization of natural resources lead to the sharp decrease of runoff volume and shrink of the lake area . the ebinur lake area change converses from the condition subordinate to nature to human activity
    即第一阶段: 20世纪50 80年代末,此阶段由于人类对自然规律认识的局限性,以及人口增长造成的需求增长,不合理利用水土等自然资源,导致入湖水量剧减,艾比湖呈现急剧缩小的趋势,湖面变化从受控于自然条件向受控于人类活动方向转变。
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