1) clay dissolution
粘土溶蚀
2) sub-soil dissolution
土下溶蚀
1.
An intensive sub-soil dissolution zone,brought about by the harmonious working of soil CO2 and soil water,makes stone forest higher and higher,and the bottom line for the .
土壤CO2和土壤水组合形成的土下强溶蚀带的存在使得石林通过土下溶蚀不断增长拔高,但溶蚀下限一般在土下10m以内。
3) soil corrosion
土壤溶蚀
4) swelling clay
溶胀粘土
1.
Based on determinations of swelling clays from German and domestic "Jianping" clays,bentonites suitable for preparing high performance swelling clays were screened out from bentonites occured in different areas.
本文通过对德国溶胀粘土以及国内建平商品土性能测定,针对国内不同产地的膨润土,筛选适宜制备高性能溶胀粘土的膨润土样品;并通过提纯、改型和复配试验,研制出性能基本符合德国产品的溶胀粘土。
5) clay alteration
粘土化蚀变
6) Clay-alteration
粘土类蚀变
补充资料:孤峰溶蚀平原
孤峰溶蚀平原是指峰林平原进一步发育,峰林不断溶蚀降低,地表夷平,仅有少量山峰存在所形成的平原
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条