生物风化的英文

• biologic weathering
• biological weathering
• biologicalweathering
• organic weathering

• "生物"英文翻译    living things; living beings ...
• "风化"英文翻译    morals and manners; decency
• "生物风化作用" 英文翻译 :    organic weathering
• "矿物风化序列" 英文翻译 :    weathering sequence of mineral
• "生物风险" 英文翻译 :    bioventure
• "有害生物风险分析" 英文翻译 :    risk analysis for alien pests
• "风化" 英文翻译 :    1.(风俗教化) morals and manners; decency 有伤风化 an offence against decency2.[化学](化合物失去结晶水) efflorescence3.[地] (地壳表面岩石在大气、水和生物等长期作用下发生破坏或变化) weathering; air-slake
• "谷物风干室" 英文翻译 :    barn for drying crops
• "谷物风选机" 英文翻译 :    grain fanning-sorting machine
• "风化作用；风化" 英文翻译 :    weathering
• "胡椒科植物风藤" 英文翻译 :    piper kadsura ohwi
• "风化；潮解" 英文翻译 :    air slaking
• "风化；粉化" 英文翻译 :    efflorescence
• "风化边" 英文翻译 :    weathering rind
• "风化冰" 英文翻译 :    weathered ice
• "风化材" 英文翻译 :    seasoned wood
• "风化槽" 英文翻译 :    weathering trough
• "风化层" 英文翻译 :    alteration mantle; c horizon; chorizon; mantle of rock; mantle of soil; mantle rock; overburden; reglith; regolith; rock mantle; solum; waste mantle; weather layer; weathered crust; weathered horizon; weathered layer; weathered zone; weatheredlayer; weathering layer; zone of weathering
• "风化带" 英文翻译 :    belt of weathering; weathered zone; weathering belt; weathering zone; zone of weathering; zoneofweathering
• "风化的" 英文翻译 :    efflorescent; slack; weathered
• "风化度" 英文翻译 :    degree of weathering; weathering grade
• "风化监" 英文翻译 :    effflorescent salt
• "风化壳" 英文翻译 :    crust of weathering; crustofweathering; residuum; weathered crust; weathered mantle; weathering crust; weatheringcrust
• "风化砾" 英文翻译 :    weathered pebble
• "风化力" 英文翻译 :    weathering capacity

• This suggests that the optimum for biological weathering would be in a hot, moist climate .
  这表明生物风化最适宜的条件是湿热气候。
• Recent development in bio - weathering research
  生物风化作用研究进展
• The main results are following : ( 1 ) the variation of clay / silt ratio can indicate the secondary clay action of dust depositions ; the variations of magnetic susceptibility and total fe content are inferred to be records of the changeable intensity of bio - pedogenesis ; the variations of sr content and rb / sr ratio can indicate bio - pedogenesis , dissolving and leaching action ; the content of total organic carbon ( toc ) can reflect variation of climate and vegetation during soil formation , it indicates the intensity of weathering and bio - pedogenesis ; the content variation of caco3 can show the intensity of dissolving - leaching action and secondary deposit , which was noted as pseudomycilia in pores and fissures in the sediment , so it can indicate the intensity bio - pedogenesis quite well . these proxy indexes also reflect obvious regional difference of pedogenic environment and the intensity bio - pedogenesis ; namely , secondary clay action , dissolving - leaching action and bio - pedogenesis are all much stronger in south than that in north
  实验结果表明：粘粒粉沙比值能很好地指示粉尘堆积物的次生粘化作用；磁化率和全铁很好地指示生物风化成壤作用； sr和rb sr比值能很好的指示生物风化成壤作用和淋溶作用；总有机碳( toc )含量的高低，在一定程度上反应了土壤发育过程中气候和植被状况的变化，指示着成壤过程中腐殖质化的程度； caco3含量的变化，可以反映了黄土古土壤形成时的风化成壤作用的强弱程度，指示成壤过程中的淋溶作用和次生碳酸盐化作用；并且各指标所指示的成壤环境和成壤强度存在明显的区域差异，即渭河流域土壤的生物风化成壤作用、次生粘化作用和淋溶作用均表现出南部强于北部。