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冻结水分
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  frozen water content
     Concludes from the investigation into the frozen coal during transportation by rail in winter, the use of defrost garage, and manual unloading of frozen coal, etc, and the analysis of major causes for frozen coal that it is an effective way to avoid frozen coal to dehydrate coal at its source to frozen water content′ in winter.
     通过对火力发电厂冬季铁路运煤发生冻煤车结冻及解冻库使用人工卸冻煤等情况的调查和对冻煤车冻煤产生的主要原因的分析 ,提出了在煤源点将煤脱水到“冻结水分”是解决冬季煤车冻煤的有效途径。
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  “冻结水分”译为未确定词的双语例句
     4) The electrical conductivity of meat is relative to musculature direction in electrical field.
     4)肉的电导率与肌肉纤维在电场中的方向有关,肌肉纤维平行于电场方向时的电导率高于垂直电场时的电导率; 冻肉的电导率与肉内不冻结水分含量有关。
短句来源
     The change of soil moisture is divided as four periods which are water consuming period in spring,water supply period in the beginning of rainy season,water fluctuation consuming period,frozen water steady sinking period in winter,respectively.
     土壤湿度在年内可分为春季水分消耗期、雨季初水分补给期、水分波动消耗期和冬季冻结水分稳定聚集期。 在垂直方向随深度加深湿度逐渐降低 ,北坡极为明显 ,南坡及滩地降低幅度均匀。
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  相似匹配句对
     The Underground Water Migration and Consolidation Effect of the Frozen Soil
     冻结土体的水分迁移和固结作用
短句来源
     5. Simulation of the water movement in the earth during freezing season;
     5.冻土冻结期间土壤水分的运动;
短句来源
     and water;
     水分:31。
短句来源
     Freeze concentration
     冻结浓缩
短句来源
     the water volatility of the resin was small;
     水分挥发性小;
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  frozen water content
Measurements of the thickness of the fog layer over the city and of the frozen water content of ice fog for various visibilities are needed for additional verification of the calculations.
      


This paper deals with the laws of seasonal and vertical changes of soil moisture in the current planting system. Four distinct stages of soil water regime are recognized, the slow lossing of soil moisture from Sep. to Nov.; the stable of soil moisture in the freezing time; the rapid lossing stage of soil moisture from April to Ju'ne and the storing stage of soil moisture from June to Aug..Vertical change of soil moisture in 0-100cm can be divided into three layers: the active layer(0-20cm), the secondary active...

This paper deals with the laws of seasonal and vertical changes of soil moisture in the current planting system. Four distinct stages of soil water regime are recognized, the slow lossing of soil moisture from Sep. to Nov.; the stable of soil moisture in the freezing time; the rapid lossing stage of soil moisture from April to Ju'ne and the storing stage of soil moisture from June to Aug..Vertical change of soil moisture in 0-100cm can be divided into three layers: the active layer(0-20cm), the secondary active layer (20-60)and the relative stable layer with good moisture(60-100).

本文研究了土壤水分的季节变化和垂直变化。土壤季节变化可划为4个时期:秋季缓慢蒸腾消耗期(9-11月)、冬季冻结水分相对稳定期(11-翌年3月)、春季初夏返浆蒸发水分强烈消耗期(4-6月)、雨季雨水下淋水分恢复期。土壤水分垂直变化划分为3个层位即活跃层(0-20cm)、次活跃层(20-60cm)、深墒较穗层(60cm以下)。在没有补充灌溉条件下,自然降水直接影响着土壤水分状况。5月至6月份是全年最干旱时期,表层0-20cm土壤含水量为5.50%,0-100cm平均土壤含水量为22.16%,土壤干旱落后于大气干旱,冬春季土壤贮水量与同期降水量关系不大,而夏秋季降水量与1m土层贮水量有一定相关关系,降水对土壤表层及上层影响较小,而对深层土壤水分影响较大。

Concludes from the investigation into the frozen coal during transportation by rail in winter, the use of defrost garage, and manual unloading of frozen coal, etc, and the analysis of major causes for frozen coal that it is an effective way to avoid frozen coal to dehydrate coal at its source to frozen water content′ in winter.

通过对火力发电厂冬季铁路运煤发生冻煤车结冻及解冻库使用人工卸冻煤等情况的调查和对冻煤车冻煤产生的主要原因的分析 ,提出了在煤源点将煤脱水到“冻结水分”是解决冬季煤车冻煤的有效途径。

The soil moisture change of the Mat_Cryic Cambisols at different topographic position was analyaed.We can conclude that soil moisture is high,and it is north slope_land>valley plain>south slope_land at the depth of 0~6 cm .The change of soil moisture is divided as four periods which are water consuming period in spring,water supply period in the beginning of rainy season,water fluctuation consuming period,frozen water steady sinking period in winter,respectively.The soil moistrue is gradually decreased from...

The soil moisture change of the Mat_Cryic Cambisols at different topographic position was analyaed.We can conclude that soil moisture is high,and it is north slope_land>valley plain>south slope_land at the depth of 0~6 cm .The change of soil moisture is divided as four periods which are water consuming period in spring,water supply period in the beginning of rainy season,water fluctuation consuming period,frozen water steady sinking period in winter,respectively.The soil moistrue is gradually decreased from topground to bottom ground,which is showed the most significant at north slope_land,and the soil moistrre decrease is even at south slope_land or valley plain.Soil moisture with the change of season is divided an periodic part,random part,and trending part.

寒冻雏形土不同地形部位土壤湿度均有较高的水平 ,0cm~ 6 0cm整层土壤湿度北坡 >滩地 >南坡。土壤湿度在年内可分为春季水分消耗期、雨季初水分补给期、水分波动消耗期和冬季冻结水分稳定聚集期。在垂直方向随深度加深湿度逐渐降低 ,北坡极为明显 ,南坡及滩地降低幅度均匀。土壤湿度随时间的变化过程分解为周期性变化项、随机性分量项及趋势项。同时表明 ,在土壤湿度较低的南坡 ,以小嵩草等为主的草原化草甸植被类型 ;土壤湿度适中的滩地 ,多以矮嵩草为主的高寒嵩草草甸植被类型 ;湿度较高的北坡 ,多以金露梅为主的灌丛草甸植被类型 ;而在土壤湿度很高、地表长久积水的河边 ,多以藏嵩草等为主的沼泽化草甸植被类型

 
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