不同淋洗对于碱土的影响
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STUDIES ON THE EFFECT OF DIFFERENT WASHINGS ON ALKALI SOILS
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    摘要:

    美洲某些以雪水为给源的山溪的灌溉水中含鹽量极少,有时低于100 p.p.m。反之,有些灌溉水中含鹽量高达10,000 p.p.m。鹽分中主要的阳离子为钙。由于灌溉废水、排水及其他一些小溪流入河中,河水中的全鹽量以及钠离子、氧化物、硫酸鹽等的相对含量乃随之增加。灌溉水中阴离子及阳离子的百分组成大致如下[1].

    Abstract:

    When alkali soil is leached with water, the amount of calcium in water extracts is always less than in the case of normal soil. With increased dilution there is a definite increase in the amount of calcium given out, yet the quantity is not very great. When water is added in increasing amounts to the normal soil, there is no increase in pH values of the successive filtrates and the pH of the distilled water is easily obtained, whilst the pH value of the alkali soils falls very gradually to a pH of 7.6. The amount -CO3 ions in the extracts gradually decreases with concomitant decrease in pH values. The amount of bicarbonates at first increases gradually and then falls. A gradual decrease in pH values also takes place with repeated washings with distilled water.

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引用本文

S. P.米特拉,H.谢克尔.不同淋洗对于碱土的影响[J].土壤学报,1957,5(4):317-321. S. P. MITRA, HARI SHANKER. STUDIES ON THE EFFECT OF DIFFERENT WASHINGS ON ALKALI SOILS[J]. Acta Pedologica Sinica,1957,5(4):317-321.

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  • 在线发布日期: 2013-02-25
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