饱和持水量的英文

• saturation moisture capacity

• "饱和"英文翻译    saturation; saturated
• "持"英文翻译    hold; grasp
• "水量"英文翻译    water yield; the yield of wa ...
• "饱和含水量（全持水量）" 英文翻译 :    saturated moisture content
• "持水量" 英文翻译 :    moisture capacity; moisture holding capacity; moisture retention capacity; moisture-holding capacity; water holding capacity; water retaining capacity; water-holding capacity; water-retaining capacity
• "持水量；持水能力" 英文翻译 :    water-holding capacity; water-holdingcapacity
• "初始持水量" 英文翻译 :    initial detention
• "单位持水量" 英文翻译 :    specific water retention
• "根区持水量" 英文翻译 :    root space capacity
• "含持水量" 英文翻译 :    moisture capacity
• "毛管持水量" 英文翻译 :    capillary moisture capacity
• "毛细持水量" 英文翻译 :    field-carrying capacity
• "田间持水量" 英文翻译 :    field capacity (field moisture capacity); field capacity （field moisture capacity）; field moisture capacity (foeld capacity); field moisture capacity （foeld capacity）; field water capacity; fieldcapacity（fieldmoisturecapacity）; fieldmoisturecapacity（foeldcapacity）
• "土壤持水量" 英文翻译 :    moisture-holding capacity; soil retention; soilretention; water capacity
• "有效持水量" 英文翻译 :    effective water-holding capacity; usable capacity
• "正常持水量" 英文翻译 :    normal moisture capacity; normal water capacity
• "最大持水量" 英文翻译 :    full water capacity; maximum moisture capacity; maximum water holding capacity; maximum water-holding capacity; water retaining capacity
• "最低持水量" 英文翻译 :    minimum water capacity
• "最后持水量" 英文翻译 :    final retention
• "最适持水量" 英文翻译 :    optimum water capacity
• "最小持水量" 英文翻译 :    least water-holding capacity; minimum water capacity; minimum water holding capacity; minimum water-holding capacity
• "持水量；保水能力" 英文翻译 :    water retention capacity; waterretentioncapacity
• "持水量；含水量；含水率" 英文翻译 :    humidity ratio
• "田间土壤持水量" 英文翻译 :    field-moisture capacity
• "田间最大持水量" 英文翻译 :    field maximum moisture capacity; maxmun field capacity

• Although the biomass and yield of rice had been hardly affected by soil moisture content , when it was 80 % or 100 % of saturated water content ( swc ) , but markedly by soil moisture content 60 % of swc
  土壤含水量为饱和持水量的60 %时对旱作水稻生物量和产量影响较大，而80 %和100 %时几乎没有影响。
• In order to gain higher yield of rice , it is essential to pay attention to p application or take some measures to improve soil p utilization efficiency
  这说明控制土壤水分为饱和持水量的80 %时就能完全满足旱作水稻的生长，但要求获得较高的产量时必须注意磷肥的投入，或者采取一些调控措施提高土壤磷的利用率。
• After yearly burning , soil moisture content , porosity , separate coefficient , capillary and field moisture capacity increased , however , soil saturated water retaining capacity and unit weight decreased
  连年火烧使土壤含水率、孔隙度、分散系数、毛管持水量和田间持水量升高，而使土壤饱和持水量、容重下降。
• The effects of forest fires on soil moisture content , separate coefficient , porosity , water - retaining capacity , organic matter , available n , available ca , fungi and fine root significantly varied between the years after burning . the effects of forest fires on soil separate coefficients , porosity , saturated water - retaining capacity , available mg , fine root significantly varied between the fire intensity
  火烧后年限对土壤含水率、分散系数、孔隙度、持水量、有机质、有效氮、有效钙、真菌、细根系生物量的影响有显著差异；火烧强度对上壤分散系数、孔隙度、饱和持水量、有效镁、细根系生物量的影响有显著差异。
• With increase of artificial forest age , the content of soil organic matter decreased sharply . and soil physical , chemical and biological properties of forest became worsen . from soil physical properties analysis , soil silt , clay , physical clay , aggregate degree and structure coefficient in topsoil increased with increase of artificial forest age and soil sand deceased
  在土壤物理性质方面，随着人工云杉林龄的增加，土壤表层粉粒、粘粒、物理性粘粒、团聚度和结构系数降低，砂粒含量增高，土壤饱和持水量、毛管持水量及总孔隙和毛管孔隙在人工云杉演替过程中表现出“ u ”型变化。
• Soil saturated capacity , capillary capacity , total porosity and capillary porosity showed the trend of the " u " during the successional course of artificial forest , namely , they reduced on the early successional stages , after picea reached mature forest , soil porosity recovered slowly . the content of natural water was mainly affected by capillary porosity . from soil chemical properties analysis , the content of soil organic , humus , ha , fa and ha / fa of topsoil was more than that of bottom layer
  即人工云杉幼林向成熟林演替阶段，土壤饱和持水量、毛管持水量及总孔隙和毛管孔隙则减少，在40年生云杉林达最低值，之后随着云杉自疏，微生态改善，林地凋落物分解加快，土壤饱和持水量、毛管持水量及总孔隙和毛管孔有上升的趋势，毛管持水量是决定林地自然含水量的主要因子。
• At the same time , the quality of different - state water was studied . the results show : the soil bulk density of the fir wildwood heightens with the increase of soil depth , specifically 0 . 74 > 0 . 94 andl . 34g / cm3 , the saturated , canaliculus and field moisture contents decrease gradually in layer a , b and c , accordingly the soil total foveola decreases gradually , and the moisture - hold capacity of the soil lessens gradually with the increase of the soil depth ; there is small difference of the soil bulk density between layer a and b in the outer space , which are respectively 0 . 92 and 0 . 99g / cm3 , and the other laws are the same as the in ner in the main ; reverse success often occurs in the low position of the thoroughly - fell trace and plateau marsh is formed
  结果表明：冷杉原始森林土壤容重随土层深度的增加而增大，分别为0 . 74 、 0 . 94 、 1 . 34g cm ~ 3 ，饱和持水量、毛管持水量、田间持水量a层、 b层、 c层逐渐减小，十壤总孔隙度也逐渐减小，土壤的持水能力随深度的增加逐渐减弱；林外空地a层、 b层十壤容重相差不人，分别为0 . 92和0 . 99g cm ~ 3 ，其它规律与林内人体相同：皆伐迹地的低洼地段容易发生逆行演替，形成高原沼泽地。