These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.
结果表明,该地区全新世大暖期古土壤为温湿气候条件下发育
淋溶褐土,
非过去所称
半干旱条件下发育
“黑垆土”.
These materials reveal that Holocene paleosol around Xi′an formed during Megathermal is luvic cinnamon soil developing in warm and humid climate but not developing in subarid climate.
结果表明,该地区全新世大暖期古土壤为温湿气候条件下发育
淋溶褐土,
非过去所称
半干旱条件下发育
“黑垆土”.
声明:以上例句、词性分类均由互联网资源成,部分未经过人工审核,其表达内容亦不代表本软件
观点;若发现问题,欢迎向我们指正。