期刊文献+
共找到1篇文章
< 1 >
每页显示 20 50 100
Characterization of Gleyization of Paddy Soils in the Middle Reaches of the Yangtze River 被引量:12
1
作者 PAN SHUZHENG(Institute of Soil Science,Acodemia Silica,Nanjing 210008 China) 《Pedosphere》 SCIE CAS CSCD 1996年第2期111-119,共9页
The gleyisation of representative paddy soils in the middle reaches of the Yangtze caver was characterized,taking oxidation-reduction potential(Eh),the amount of active reducing substances and the forms of iron and ma... The gleyisation of representative paddy soils in the middle reaches of the Yangtze caver was characterized,taking oxidation-reduction potential(Eh),the amount of active reducing substances and the forms of iron and manganese as the parameters.The Eh value was linearly related with the logarithm of the amount of active reducing substances, which was contributed by ferrous iron by 83% on an avers.The degree of gleyization of dament horizons was graded as ungleyed,slightly gleyed,mildly gleyed and gleyed.The Eh of the four grades was>500,300-500,100-300 and<100 mV,respectively, and the corresponding amoks of active reducing substances was<1,1-7,7-30 and>30 mmol.kg(-1),respectively.The amount of ferrous iron of the four grades was<0.5,0.5-5,5-25 and > 25 mmol kg-1,respectively.The extent of gleyisation of a soil was classified as upper-gleyed, middle-gleyed and lower-gleyed, depending on whether the depth of the gley horbon was less than 30 cm,30-60 cm or more than 60 cm. 展开更多
关键词 ferrous iron gleyization paddy soil reducing substances oxidation-reduction potential
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部