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sediment index中文是什么意思

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  • ( iii ) by c - 14 dating , size and sediment indexes analysis , the malan loess is studied which is the main component of the second terrace in csmasp
    認(rèn)為張夏黃土與青州黃土具有相似的成因和物源,但與洛川等地的典型黃土和萊州灣沿岸的陸架黃土有明顯差異。
  • It is indicated that the loess was mainly formed in late epipleistocene . and its sediment indexes can be compared with that of loess plateau roughly , though they have different formation causes and provenance
    研究表明,二級(jí)階地形成于13000 8500abp ,一級(jí)階地形成于4000 500abp ,河漫灘是現(xiàn)代河流作用的產(chǎn)物。
  • Many studies had attempted to characterize chemical weathering process by focusing on geochemisty of river particulate and sediment . the sediment geochemistry may reflect and compare with the carbonates and silicates weathering degree by introducing the chemical index of alteration ( cia ) and new sediment index of variation ( siv ) and elemental molar abundance ratio of the sediment . the one main objective of this study would provide and compare the relative weathering intensities of silicates and carbonates with the different basins
    2沉積物地球化學(xué)與化學(xué)風(fēng)化進(jìn)程和機(jī)械剝蝕率化學(xué)風(fēng)化指數(shù)與化學(xué)風(fēng)化率屬于表征化學(xué)風(fēng)化作用意義不同的函數(shù),前者為相對(duì)概念反映流域巖石在原巖基礎(chǔ)上己發(fā)生淋溶作用的深度,主要受到了氣候因子的深刻影響(中國流域沉積物化學(xué)風(fēng)化指數(shù)由北到南呈有規(guī)則的遞增序列,氣候因子對(duì)風(fēng)化進(jìn)程的影響掩蓋了巖性的巨大差異) ,而化學(xué)風(fēng)化率含義是指單位流域面積巖石風(fēng)化淋溶產(chǎn)生的離子絕對(duì)總量。
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