soil evaporation中文,soil evaporation的意思,soil evaporation翻译及用法

2026-04-14 08:36 浏览次数 18

soil evaporation

英[sɔil ɪˌvæpəˈreɪʃən]美[sɔɪl ɪˌvæpəˈreʃən]

土壤蒸发

soil evaporation 片语

片语

soil water evaporation土壤水蒸发

soil surface evaporation土面蒸发

soil potential evaporation土壤潜在蒸发

Soil Evaporation Parameter蒸发参数

the soil evaporation coefficient土壤蒸发系数

soil moisture evaporation土壤水分蒸发的

soil evaporation observation土壤蒸发观测

soil evaporation between plants棵间蒸发

soil evaporation 例句

英汉例句

  • the quantitative calculation method of soil evaporation is widely applied in the water conservancy, hydrology, agriculture, ecology, environment, geography and meteorology etc.

    土壤蒸发定量计算方法在水利、水文、农业、生态、环境、地理、气象等方面有广泛的应用基础。

  • with restoration ecology as a guide, a soil evaporation experiment was conducted to analyze the effects of different material covers on soil moisture in the typical steppe zone.

    通过在希拉穆仁草原典型地带进行不同材料覆盖的土壤蒸发实验,并以恢复生态学为指导思想,研究了不同材料覆盖对土壤水分的影响。

  • it contains soil evaporation and plant transpiration.

    蒸散包括土壤蒸发和植被蒸腾。

  • the soil evaporation from the highest to the least was turf soil, coal cinder, ck, sand, sawdust and smash of straw successively.

    不同覆盖物下土壤蒸发量差异显着,白天影响蒸发量大小的覆盖物依次是草炭土、煤渣灰、裸地、对照、河沙、锯末、豆秸。

  • precipitation, soil evaporation and plant transpiration were the primary factors affecting soil moisture which variation with time.

    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。

  • the effect of restraining soil evaporation by litter is quite small when the water content in soil is less than 11%.

    当土壤水分低于11%时,枯枝落叶层抑制土壤蒸发的作用很小。

  • no tillage with mulch could reduce soil evaporation and increase crop transportation, which was important for water saving agriculture.

    从蒸发占蒸散的比例看,翻耕蒸发比例高,免耕比例最低。免耕可以有效地减少土壤蒸发量,增加作物蒸腾耗水。

  • 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…

    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。

  • this article overviews several documents about soil evaporation in the last several decades. in the end, the paper presents the significance of soil evaporation study on drought prevention and cure.

    本文综述了几十年来土壤蒸发研究基本理论及发展过程,并提出了对于旱灾防治的意义。

  • so the more precipitation does in the region , the more soil evaporation and transpiration of plant is more much, evapotranspiration in year of abundant precipitation is great than level year.

    所以说在该地区降雨量越多,土壤蒸发和植物蒸腾越大,丰水年的蒸散量要大于平水年的蒸散量。

  • calculation of quantity of soil evaporation takes an important part in moisture content prediction, rainfall surface flow calculation and evaluation of water resources.

    土壤蒸散发量的计算,在墑情预报、降雨径流计算及水资源评价中都占有重要的地位。

  • landfill leachate can be greatly reduced through soil evaporation under the recycling irrigation.

    通过循环蒸发处理,垃圾渗滤液可以大量削减。

  • air-dry soil surface evaporation represents the lower limit of soil evaporation under the same weather, for the quantity of evaporation is zero under the any weather.

    饱和土壤表面,代表了相同气象条件下土壤蒸发的上限,其蒸发在任何气象条件下都为土壤的可能最大蒸发;

  • iii, with the development of remote sensing temperature technique, there will be superiority in calculating soil evaporation on large area.

    随着遥感测温技术的发展,这些模型在计算大面积范围的土壤实际蒸发时,将会体现出一定的优越性。

  • it has two parts, soil evaporation and plant transpiration.

    包括土壤蒸发和植物蒸腾两部分。

  • in the end, the paper presents the significance of soil evaporation study on drought prevention and cure.

    本文综述了几十年来土壤蒸发研究基本理论及发展过程,并提出了对于旱灾防治的意义。

  • soil evaporation and moisture and heat transport are important constitutes of energy and water balance of soil surface.

    土壤蒸发与水热传输是地表能量与水分平衡的重要组成部分。

  • field water consumption (evaportranspiration, et) consists of crop transpiration (t) and soil evaporation (es).

    冬小麦农田耗水包括作物蒸腾与棵间土壤蒸发两部分。

  • make the method of principal component analysis to the study of meteorological factors research for sandy soil evaporation capacity , give three main factors to impact sandy soil evaporation capacity;

    将主成分分析法用于沙地土壤蒸发能力的影响因子的分析中,影响沙地土壤蒸发能力的各因子归结为三个主成分;

  • the soil evaporation between different section of slope has no significant difference.

    不同坡位间的土壤蒸发没有显着差异。

  • because of the shading of wood leaf layers and litter fall, soil evaporation and the range of soil moisture contents changing were small under forest canopy.

    受冠层覆盖及植被根系影响,随着树干距离的增加,土壤含水率呈减少趋势。

  • furthermore, the diurnal variation of soil evaporation and crop transpiration shows that two interfaces interact with each other on energy and vapor transition.

    通过不同时期日蒸散发量变化特征的分析,表明土壤、冠层两个界面对能量和水汽传输的交互影响效应显着。

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