1) soil chronosequence
土壤序列
1.
Soil development indices(SDIs)quantified by soil morphological characteristics were used to es- timate the development degree of the soil chronosequence on recessional moraines of Hailuogou Glacier in the Gongga Mountain.
剖面发育指数(PDI)和加权平均剖面发育指数(WPDI)作为剖面累积发育指标,可以用于不同土壤序列的发育速率比较。
3) loess-paleosol sequence
黄土-古土壤序列
1.
Element distributions of the Zhuanglang Holocene loess-paleosol sequence,Gansu Province and its significance;
甘肃庄浪全新世黄土-古土壤序列元素分布特征及意义
2.
In Nanyuan of Jingyang (34°28 N and 108°53 E)and Xiwang of Xi an (34°17 N and 109° 04 E), Guanzhong, Shaanxi Province, the Late Pleistocene loess-paleosol sequence is best preserved and typical in the Loess Plateau of China at present.
这是目前发现的黄土高原晚更新世黄土-古土壤序列保存较好的剖面。
3.
The loess-paleosol sequence of the Chinese Loess Plateau is formed on the condition of dry and cold climate to warm and humid climate altenately, during dust depositing and soil -forming process in the glacier-interglacier cycle in Quaternary.
我国黄土高原的黄土-古土壤序列,是在第四纪时期全球冰期-间冰期旋回背景上,古气候条件冷干-温湿的周期性变化下进行的风尘沉积-成壤过程的产物。
4) loess/palaeo soil series
黄土古土壤序列
5) loess-paleosol series
黄土-古土壤地层序列
6) Quaternary loess-paleosol sequence
第四纪黄土-古土壤序列
补充资料：土壤水分运动基本方程(见土壤水运动)
土壤水分运动基本方程(见土壤水运动)
turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
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