Plants in green roofs regulate their temperatures through evapotranspiration.
植物通过水分蒸发调节绿色屋顶的温度。
Evapotranspiration may deplete the soil moisture and rob supplies of ground water.
蒸发蒸腾作用能消耗土壤水分，减少地下水的水量供应。
Other things being equal, the evapotranspiration rate decreases with increasing humidity.
当其它条件相同时，蒸散率随湿度增大而减小。
The large planted surface area stimulates evapotranspiration, which helps keep visitors nice and cool.
亭子上大片的植被覆盖面起到蒸发蒸腾作用，这样亭子里的游客会感觉舒适凉爽。
Soil water deficit is the main limiting factor affecting the growth and evapotranspiration of spring wheat.
土壤水分条件的恶化是影响春小麦生长和蒸发蒸腾的主要限制因子。
The forest, by recycling the water that falls on it through evapotranspiration, plays an important part in this system.
由于通过蒸腾作用来循环那些降入丛林中的水，森林在上述系统中发挥了相当重要的作用。
Weighted average method is used to study the soil cover′s effect on the evapotranspiration in irrigated watershed.
利用灌区下垫面分类明显的特点，用加权平均法解决下垫面对流域蒸散发的影响；
The system provides calculation of crop evapotranspiration and irrigation quota, and introduces many irrigation methods.
提供了作物需水量计算、灌水定额计算，并且介绍了各种灌水方法。
The results exhibited that (1) soil moisture and evapotranspiration were closely relative to vegetation types and rainfall.
研究结果表明：（1）土壤含水量、蒸散量均与植被类型和降雨量密切相关。
It is based on actual evapotranspiration capacity, effective rainfall and water reserve of soil to forecast irrigation time.
以实际蒸发蒸腾量、有效降雨量和土壤贮水量来预报未来灌水时间。
The results showed that the evapotranspiration was the main form of water output in the upper reaches of Raoyang River Watershed.
结果表明，绕阳河上游流域水量平衡中蒸散是水分输出的主要形式。
When the stability is weak, in some conditions, the solutions of evapotranspiration rate can appear in a multi-equilibrium state.
研究还发现，绿洲中总的蒸散量的多平衡态特征只有在稳定度低的时候出现。
The research results provided an effective method for the distributed rainfall-runoff model in simulating actual evapotranspiration.
为流域分布式降雨-径流模型提供了可靠的实际蒸散量模拟方法。
This article makes use of the Bowen Ratio-equilibrium Energy Method to measure evapotranspiration of Tamarix ramosissima in Ejina oasis.
利用波文比能量平衡法对额济纳绿洲柽柳种群蒸散进行测定。
In rainy year, soil water storage increased, but most infiltrated rainfall (more than 80%) was consumed by intensive evapotranspiration.
丰水年，土壤水分收支正平衡，但入渗雨量的大部分（>80%）为强烈蒸发蒸腾所消耗。
The results showed that the reference crop evapotranspiration in Hunpu irrigation district increased first and then decreased gradually.
结果表明，在生育期内浑蒲灌区参考作物需水量的变化规律表现为先增大后逐渐减小。
The result of application shows that the simulation of soil water dynamics and evapotranspiration by using the model has high precision.
经初步应用结果表明，该模型模拟无地下水补给条件下玉米田土壤水分动态具有较高的精度。
The quantity of evapotranspiration of crops is limited by soil moisture deficits, in different growth period, the influences is different.
作物腾发量受土壤水分亏缺的制约，在不同的生长阶段，影响的大小亦不同。
This paper reviewed the methods for computing crop water requirements and emphasized the method based on reference crop evapotranspiration.
评述了作物需水量的计算，并着重分析了基于参考作物蒸发蒸腾量计算作物需水量的方法。
The impacts of climate on potential evapotranspiration and soil water content under 2080's climatic condition were simulated with the model.
还利用建立的模型，模拟了2080年的气候条件变化对潜在蒸散量和土壤水分含量的影响。
Potassium dihydrogen phosphate promoted the opening of stomates so as to increase evapotranspiration intensity and relative water loss rate.
磷酸二氢钾有促进气孔开张的作用，使蒸腾强度和相对失水率相应增大。
Using the PE Model, the canopy photosynthesis, evapotranspiration and water use efficiency (WUE) for different rice plant types were simulated.
利用PE模型，分别模拟了水稻前中期与后期不同株型的群体光合量、蒸散量以及水分利用效率。
In the condition of limiting irrigation situation, the evapotranspiration of turf-grass species were obviously less than sufficient irrigation.
充分灌水和限制灌水两种条件下，冷季型草坪草年蒸散量大于暖季型草坪草年蒸散量。
The micrometeorological methods for calculating evapotranspiration, which not destroy ground surface, can be used to measure an even formed stand.
微气象学法不破坏下垫面，适用于整齐均一的作物与林木蒸散的测定；
Plants give off water through tiny pores in their leaves, a process called evapotranspiration that cools the plant, just as perspiration cools our bodies.
植物通过其叶子上的微细小孔排出水分，这个蒸发过程使植物降温，就好像流汗使我们凉快一样。
The Zero Flux Plane (ZFP) principle and method are applied to study the farmland evapotranspiration in Beijing Fangshan water-saving irrigation area.
应用土壤水分零通量面的原理方法，对北京房山节水灌溉区进行了研究。
Of all components of water balance in farmlands, evapotranspiration, capillary rise from a water table and deep percolation are difficult to determine.
在农田水分平衡中，较难测定的要素有农田蒸腾蒸发量、地下水毛细上升量和土壤水渗漏量。
Analysis of the effects of soil, plant and atmospheric factors on the calculation of evapotranspiration is made on the basis of field experimental data.
本文从田间实验资料入手，逐一分析了土壤、植物、大气因子对蒸散计算的影响。
Analysis of the effects of soil, plant and atmospheric factors on the calculation of evapotranspiration is made on the basis of field experimental data.
本文从田间实验资料入手，逐一分析了土壤、植物、大气因子对蒸散计算的影响。
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