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从上表看出,冲洪积平原中的氟元素含量远比剥蚀平原中的含量要高,前者是后者的5倍以上。其它元素除Mg、Se、Sr以外,在两种地貌单元上的含量差别非常小,而Mg、Se、Sr在...
从上表看出,冲洪积平原中的氟元素含量远比剥蚀平原中的含量要高,前者是后者的5倍以上。其它元素除Mg、Se、Sr以外,在两种地貌单元上的含量差别非常小,而Mg、Se、Sr在冲积-洪积平原的含量分别为剥蚀平原含量的近2倍、2倍和4倍。四种元素之间的相关关系十分显著。高密市北部地区较大的河流只有胶莱河一条,整个冲积洪积平原地区蒸发作用强烈,地下水主要通过蒸发和蒸腾进行排泄,地下水中的氟随毛细作用上升至浅表土壤,降雨时被淋虑至地下水中,如此反复很容易使地下水中的氟含量因为浓缩而增高。
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从上表看出,冲洪积平原中的氟元素含量远比剥蚀平原中的含量要高,前者是后者的5倍以上。Seen from the table above, the fluorine content in the alluvial proluvial plains is higher than that in the denudative plains, about 5 times as much as the latter.
其它元素除Mg、Se、Sr以外,在两种地貌单元上的含量差别非常小,而Mg、Se、Sr在冲积-洪积平原的含量分别为剥蚀平原含量的近2倍、2倍和4倍。四种元素之间的相关关系十分显著。
The content of the other elements, except Mg, Se and Sr, is of little difference between the two kinds of geomorphologies. However, the content of Mg, Se, and Sr in the alluvial proluvial plains is respectivly twice, twice and four times as much as that in the denudative ones. There seems to be an obvious correlativity among these 4 elements.
高密市北部地区较大的河流只有胶莱河一条,整个冲积洪积平原地区蒸发作用强烈,
There is only one river, Jiaolai River, which can be called larger, in the north of Gaomi City. A strong evaporation occurs in the entire alluvial proluvial plains.
地下水主要通过蒸发和蒸腾进行排泄,地下水中的氟随毛细作用上升至浅表土壤,降雨时被淋虑至地下水中,如此反复很容易使地下水中的氟含量因为浓缩而增高。
The ground water discharge mainly in the ways of evaporation and transpiration. The fluorine in the ground water rises to the near-surface layers of the soil with the capillarity, while eluviates down to the ground water again when it rains. Over again and again the fluorine in the ground water tends to concentrate to enrichment.
其它元素除Mg、Se、Sr以外,在两种地貌单元上的含量差别非常小,而Mg、Se、Sr在冲积-洪积平原的含量分别为剥蚀平原含量的近2倍、2倍和4倍。四种元素之间的相关关系十分显著。
The content of the other elements, except Mg, Se and Sr, is of little difference between the two kinds of geomorphologies. However, the content of Mg, Se, and Sr in the alluvial proluvial plains is respectivly twice, twice and four times as much as that in the denudative ones. There seems to be an obvious correlativity among these 4 elements.
高密市北部地区较大的河流只有胶莱河一条,整个冲积洪积平原地区蒸发作用强烈,
There is only one river, Jiaolai River, which can be called larger, in the north of Gaomi City. A strong evaporation occurs in the entire alluvial proluvial plains.
地下水主要通过蒸发和蒸腾进行排泄,地下水中的氟随毛细作用上升至浅表土壤,降雨时被淋虑至地下水中,如此反复很容易使地下水中的氟含量因为浓缩而增高。
The ground water discharge mainly in the ways of evaporation and transpiration. The fluorine in the ground water rises to the near-surface layers of the soil with the capillarity, while eluviates down to the ground water again when it rains. Over again and again the fluorine in the ground water tends to concentrate to enrichment.
2012-04-17 · 知道合伙人金融证券行家
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From the above table shows
沙发同志,你上来就是个语法错误啊。你这不是坑害楼主嘛。。。。
沙发同志,你上来就是个语法错误啊。你这不是坑害楼主嘛。。。。
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From the above table shows, alluvial plain in the element fluorine content than the plain of denudation in the content to be high, the former is the5 times above. Other elements except for Mg, Se, Sr beyond, in two kinds of landform unit content difference is very small, but Mg, Se, Sr in the alluvial - flood plain content respectively denudation plain content of nearly 2 times,2times and 4 times. Four the correlation between the mineral is very significant. Northern Gaomi City region of the larger rivers only Jiaolai river a, the alluvial flood plain area, strong evaporation, groundwater mainly through evaporation and transpiration of excretion, groundwater fluorine with capillarity rise to superficial soil, rain drench the worry to groundwater, so it is easy to make the fluorine content in groundwater as the concentration increases
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