片语

Soil & Water Science变脏

soil-water recharge土壤水份补充

soil-water resources土壤水资源

conserve soil and water保持水土

soil-water belt土壤水带

soil-water conservation水土保持

Soil and Water Science土壤和水科学

soil capillary water[土壤]

英汉例句

• in control condition of the growth chamber analyzing the influence of inoculum density, soil water matric potential and soil temperature on mortality of pepper caused by p.

  在生长箱内控制条件下分析测定了接种体密度、土壤水分基质势和土壤温度对辣椒疫病死苗率的影响。

• the pipes can be divided into four kinds based on their cause of formation, namely pipes formed by the animals, by the roots of plants, by the cracks of soil and by the soil water movement.

  根据土管成因不同将其分为四种类型，即土壤动物活动导致的土管、植物根系形成的土管、土壤裂隙形成的土管和土壤水分运动形成的土管。

• build the correlation between soil water content and topography of intertidal flat through statistics , and simulate the topography of intertidal flat in dafeng.

  通过统计方法，建立出露潮滩土壤水分与实测潮滩地形的相关关系，并对大丰港堤附近潮滩地形进行了反演。

• a field experiment was conducted to study effects of root pruning at returning green stage on population structure, soil water and yield formation of winter wheat.

  通过田间试验研究了返青期不同程度根修剪处理对冬小麦群体结构、土壤水分及产量形成的影响。

• owing to the difference of soil water in the farm, variable rate irrigation can save water as well as raising economy benefit.

  依据农田内土壤含水量的差异性，有针对性地进行变量灌溉，既可节约用水又可提高经济效益。

• the non-stomatal limitation play dominant role in decline of photosynthesis while relative soil water content is below 65% which could do harm to photosynthesis organ.

  当土壤相对含水量低于65 %时，非气孔限制逐渐成为光合下降主导因子，并可能导致光合器官受到损伤。

• soil water erosion is a complex physicochemical process.

  土壤水蚀是一个复杂的物理化学过程。

• based on soil water infiltration testing and related parameters measured in field, tillage soil water infiltration capacity attenuation process was analyzed and the mechanism was discussed.

  基于大田土壤水分入渗试验与相关参数的测定，分析了耕作土壤入渗能力衰减过程，探讨了耕作土壤入渗能力衰减机理。

• study of effects of the concrete mulch on movement of soil water and soil heat transfer.

  硬覆盖对土壤水热传输及作物生长发育影响的试验研究。

• however, when precipitation rate is large enough and soil water goes beyond the field capacity, the excessive soil water will flow laterally to the lower levels through noncapillary pores.

  而当降水强度较大，以致使土壤水分大于田间持水量时，超过田间持水量部分的土壤水会很快流往较低的台阶。

• the relationship between rainfall and soil water supply is linear.

  土壤水分补给量与降雨量为线性关系；

• then it progresses relativity analysis and compare of soil water and salinity of different physiognomy positions and soil layers.

  同时对土壤水分和盐分含量在不同地貌部位和不同土壤层次进行了相关性分析与比较。

• so soil water should be analyzed as well as lime soil in the study on lime profile.

  所以，对石灰土-土壤剖面化学组成的研究应同时将土壤和土壤水加以考虑。

• effects of the influencing factors on soil water and salt movement and their mechanisms were investigated.

  得出试验因素影响因子对土壤水分盐分动态的作用及其调控机制；

• according to the differences of soil water potential in the farmland, variable irrigation can save water as well as raise economic benefit.

  依据农田内土壤含水率的差异性，有针对性地进行变量灌溉，既可节约用水又可提高经济效益。

• so this thesis regards zhangye city as study area, and quantificationally analyzes and researches spatial heterogeneity of soil water and salinity in oasis and a transition zone.

  因此本文以张掖市为研究区域，对绿洲及绿洲荒漠过渡带土壤水盐含量的空间异质性进行了定量的分析研究。

• soil water content forecast is base work for cropland irrigation timely.

  土壤水分预报是农田适时适量灌水的基础。

• it increased plough layer soil water and available nutrients content.

  大豆覆膜增加了土壤水分与速效养分含量。

• compared with conventional tillage method, the mulch tillage practice increased soil water content.

  与常规耕作方式相比，随着秸秆覆盖量增加，土壤水分增加。

• the experiment on effect of soil water on blotchy ripe ning in tomato fruit was conducted with variety jiafen no. 10 in greenhouse.

  在日光温室内，以番茄品种佳粉10号为试材，研究了土壤水分对番茄褐变型筋腐病发生的影响。

• under conventional till, crop response to spring soil water content was considerably greater than under zero till.

  在常规耕作条件下，春季作物对土壤水份含量的响应要比免耕地大得多。

• the results showed that factors influencing soil water followed a descending order of slope direction, soil, degree of slope and position of slope .

  研究结果表明，影响该地区土壤水分含量的因子按大小依次为坡向、土壤、坡度和坡位。

• it is important element of production management to control soil water content reasonably and harmonize growth between root and stem at this stage.

  合理地控制土壤水分含量，协调地上部分和地下部分的生长是此期生产管理的重要环节。

• based on field experiments and perfect model, a model of runoff and soil water balance was set up to assess the impacts of conservation tillage practices in dry land areas of northern china.

  在田间试验和对现有径流模型及土壤水分平衡模型改进的基础上，建立了适用于保护性耕作的地表径流和土壤水分平衡模型。

• the model assumed that when the soil water is smaller than field capacity, redistribution flow is negligible.

  基本假设是当土壤水分小于田间持水量时，再分配流动可以忽略。

• 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。

• lead into soil water salt dynamic model as terms of controlling, finally compile the calculation procedure among model.

  在模型中引入土壤水盐动态模型作为控制条件，最后编制了计算程序。