2) 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。
3) loess/palaeo soil series
黄土古土壤序列
4) loess-paleosol series
黄土-古土壤地层序列
5) Quaternary loess-paleosol sequence
第四纪黄土-古土壤序列
6) aeolian dust deposition paleosol sequence
风尘堆积-古土壤序列
1.
As a paleo climatic proxy index, magnetic susceptibility parameter, which has been widely used in the loess studies of northern China, is applied in the studies on quaternary aeolian dust deposition paleosol sequence located in the south of the lower reaches of the Yangtze River.
将北方黄土研究中广泛应用的磁化率参数引入江南第四纪风尘堆积区研究，对安徽宣城风尘堆积－古土壤序列向阳剖面进行了系统的磁化率化采样、测试，根据该剖面磁化率及其曲线的变化特征，对其古气候指示意义进行了初步的探讨。
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