evaporation basin 中文意思是什麼
evaporation basin
解釋
蒸發池- evaporation : n. 1. 蒸發（作用），發散，升華沉澱作用。2. 脫水（法）。3. 蒸氣。4. （電子的）發射。5. 蒸發量。6. 消散。
- basin : n 1 臉盆；水盆。2 滿盆，（一）盆。3 盆地，流域。4 水坑，地塘；（港灣）深度；內灣，小灣；【造船】...
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Conspicuously heavier hydrogen and oxygen isotopic compositions in maolouchi river basin after quake suggested that the water source of the rivulet mainly drained from surface runoff subjected to evaporation or the interflow composed with heavier isotopes
貓羅溪流域在地膿后其氫、氧同位素組成明顯變重，此意指流至河川之水源可能改變為遭受蒸發作用之地表逕流，或以具較重同位素組成之中間流為主。 -
Relationship between water surface evaporation and phreatic water evaporation when phreatic water buried depth is zero for different soil in tarim river basin
潛水埋深為零時塔里木盆地不同土質潛水蒸發與水面蒸發關系分析 -
On the platform of digital basin derived from raster dem data, - a grid - based hydrological model and a subcatchment - based hydrological model were used to study the effects of spatial variability on runoff process on such aspects as precipitation, model parameters and soil evaporation
在構建的數字流域平臺基礎上，建立分別基於子流域離散和柵格離散的數字水文模型，從而分析研究降水、模型參數和土壤蒸發的空間不均勻性對模擬水文過程的影響。 -
Variation of phreatic evaporation and its calculation method in tarim river basin in xingjiang region
塔里木盆地潛水蒸發規律與計算方法研究 -
Sedimentary evolution underwent three stages included in the evaporation sea bay of the earlier stage, shallow sea basin of the middle stage, extensive sea of the continental margin
沉積演化經歷了早期蒸發性海灣、中期淺海盆地、晚期陸緣廣海的過程。 -
The results indicated that due to the factors like relief, the evaporation capacity of chao lake basin was unbalanced in spatial distribution and appears to be on the rise on the whole during the period under discussion
研究表明，由於地形等因素的影響，巢湖流域的蒸發量空間分佈不均衡，在研究時段內蒸發量大體呈上升趨勢。 -
Based on the runoff - evaporation hydrological model the water consumption in large oases located along the kashigar, yerqiang, aksu, hetian and kaidu - kongque river in the tarim basin are analyzed
摘要應用散耗性水文模型的模擬結果，對塔里木盆地的喀什噶爾河、葉爾羌河、阿克蘇河、開都孔雀河、和田河的大型綠洲的耗水進行了綜合分析。 -
Being a typical arid inland river basin, heihe river valley, with scarce precipitation and strong evaporation, is a heavy arid region, where water resources per capita is only 1350m3 and per mu 510m3, only 60 % and 30 % of those of china
黑河流域作為我國典型的乾旱內陸河流域，不僅降雨稀少，而且蒸發強烈，人均實際佔有水資源量僅為1350m ~ 3 ，畝均水量為510m ~ 3 ，分別為全國的60和30 ，接近缺水的下限，是嚴重乾旱缺水的區域。
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