虽然海洋蒸发的水蒸气是水循环中地球表面到大气这一渠道的首要组成部分，植物蒸腾所占的部分也颇为惊人。
While evaporation from the oceans is the primary vehicle for driving the surface-to-atmosphere portion of the hydrologic cycle, transpiration is also significant.
对水源管理者来说，只有在水通过物理蒸发变成空气的一部分，或者被植物吸收并且转变为水蒸气形式(蒸腾作用)的时候，才被消耗了。
For a water manager, the only time water is consumed is when it evaporates into the air or is soaked up by plants and then turned into water vapor (transpiration).
大气层中水蒸气几乎都来源于蒸发作用、蒸腾作用、升华作用再加上火山释放的水蒸气。
Together, evaporation, transpiration, and sublimation, plus volcanic emissions, account for almost all the water vapor in the atmosphere.
在这种前提下，测量水的消耗(使用)量，即是测量物理蒸发和植物蒸腾作用的总量。
Under this definition, measuring water use comes down to measuring evaporation and transpiration, or.
但是蒸发蒸腾比汗水更难处理。
土壤含水量随时间的变化，主要受降水量和土壤蒸发与植被蒸腾耗水的影响。
Precipitation, soil evaporation and plant transpiration were the primary factors affecting soil moisture which variation with time.
以蒸发蒸腾和重力流作为土壤渗透恢复机制，建立了生物滞留槽土壤渗透与恢复过程模拟模型。
In this paper a soil infiltration and recovery simulation model of bioretention trough was constructed by using evaporation, transpiration and gravity flow as the soil recovery mechanisms.
这是因为温度升高会增加水的消耗和蒸发，植物的蒸腾也会加快。
This is because the higher temperatures will increase water consumption, evaporation and plant transpiration rates.
灌区耗水结构随着灌溉和农业耕作技术的改进，无效的蒸发、渗漏减少，有效的作物蒸腾增加。
With the improvement of irrigation and farming technique, the unavailable evaporation and seepage are reduced and the effective crop transpiration is increased in irrigation areas.
通过研究减少蒸腾蒸发(et)，来达到“真实”节水。
Through reducing the evaporation and transpiration (ET) to achieve "really" saving water.
草原群落蒸发蒸腾是一个由多种因素综合影响的复杂问题。
The evaporation and transpiration of the steppe communities is a complex problem influenced by many factors.
地表缺水指数是通过基于亚像元的双层蒸散模型提取的，它既考虑了土壤的水分蒸发，又考虑了植被的蒸腾。
The surface water deficit index is extracted based on the dual-layer evapotranspiration model, including soil water evaporation and vegetation transpiration.
在土壤蒸发、叶片蒸腾、地下入渗中PS最高，在地表径流中ps最低，这与PS的孔隙度有关。
The soil evaporation, leaf transpiration rate and surface Infiltration of PS was highest, surface runoff was lowest, relating to porosity of PS.
包括土壤蒸发和植物蒸腾两部分。
很好供水的苗木的蒸腾量与潜在蒸发量成线型相关。
The relationship between transpiration and potential evaporation was linear for well-watered seedlings.
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。
Of all components of water balance in farmlands, evapotranspiration, capillary rise from a water table and deep percolation are difficult to determine.
秸秆覆盖能抑制土壤蒸发，增强作物蒸腾，从而提高作物水分利用效率，在旱地推广合理施肥和秸秆覆盖技术是提高作物产量的有效途径。
Mulch straw could increase WUE by reducing soil evaporation and increasing crop transpiration. The yield could be increased by using the technique of rational fertilizer a...
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。
The large planted surface area stimulates evapotranspiration, which helps keep visitors nice and cool.
从日变化数据来看，植物蒸腾由于能消耗更深层次的水分，其强度的减弱要迟于土壤蒸发。
The data of daily-variety indicates the lowering of intension of plant transpiration is later than evaporation of soil surface, because transpiration can consume the deeper layer water.
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。
Soil water deficit is the main limiting factor affecting the growth and evapotranspiration of spring wheat.
土壤蒸发主要受表层土壤含水量的影响，蒸发蒸腾随作物发育进程发生剧烈的变化。
Soil evaporations are mainly affected by surface soil moisture. Evapotranspiration change from the development process.
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。
It is based on actual evapotranspiration capacity, effective rainfall and water reserve of soil to forecast irrigation time.
蒸发蒸腾作用能消耗土壤水分，减少地下水的水量供应。
Evapotranspiration may deplete the soil moisture and rob supplies of ground water.
群落生物置随牧压增大而降低是导致群落蒸发和蒸腾与牧压呈正、负相关的主要原因。
Decrement of the community biomass with the grazing pressure was the key reason for the positive and negative correlation.
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。
In rainy year, soil water storage increased, but most infiltrated rainfall (more than 80%) was consumed by intensive 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。
This paper reviewed the methods for computing crop water requirements and emphasized the method based on reference crop evapotranspiration.
选取较容易测得的重要因素，建立蒸发蒸腾量的气象因子响应模型，模拟结果较为满意。
Through factors analysis, important factors were selected, and response model was constructed. The analog result was relatively satisfied.
因此认为番茄苗期最佳补充灌溉量为植株蒸腾蒸发量的100%。
So it was concluded that the 100% ET0 supplementary irrigation was the best for the growth of tomato seedlings.
不同天气情况下，作物蒸发蒸腾量的日变化曲线基本相同，都是典型单峰型，变化的幅度、变化速率、峰值出现的时刻以及峰值的大小有差异。
The curve of evapotranspiration is the typical unimodal sort, but for the difference with the amplitude , velocity , the size and time of the maximum evapotranspiration.
不同天气情况下，作物蒸发蒸腾量的日变化曲线基本相同，都是典型单峰型，变化的幅度、变化速率、峰值出现的时刻以及峰值的大小有差异。
The curve of evapotranspiration is the typical unimodal sort, but for the difference with the amplitude , velocity , the size and time of the maximum evapotranspiration.
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