1.
Source of the Holocene Aeolian Loess-Soil in the Upper Reaches of the Huaihe River;
淮河上游全新世风成黄土—土壤物质来源研究
2.
Holocene aeolian loess and pedogenic environmental change in the upper-reaches of the Huaihe River;
淮河上游全新世风成黄土与成壤环境变化研究
3.
THE OLDEST EOLIAN LOESS DEPOSITION IN LONGXI BASIN-YANDONGGOU PROFILE IN LANZHOU
陇西盆地最老的风成黄土沉积——兰州烟洞沟剖面
4.
Substance Source of the Holocene Aeolian Loess-soil and Its Depositional Dynamics in Yuzhou, Henan Province;
河南禹州全新世风成黄土—土壤物质来源与沉积动力研究
5.
Source of the Holocene Aeolian Loess-soil in the Upper Reaches of the Yinghe River;
颍河上游地区全新世风成黄土-土壤物质来源研究
6.
A buff to gray windblown deposit of fine-grained, calcareous silt or clay.
黄土一种风沉积而成的颗粒细
7.
Most loess is considered to be an eolian deposit.
大多数黄土被认为是一种风成沉积。
8.
Aeolian-genesis comparability of aggraded red earth in south China with loess in north China;
第四纪加积型红土与黄土的风成相似性探讨
9.
Wind-deposited sediment called loess occurs in many places.
被称为黄土的风成沉积物，在许多地区均有。
10.
Loess is easy borne by the wind and may be carried long distances before it falls to earth and becomes topsoil.
黄土易被风刮起并带至远处方才落下成为表土层。
11.
However, in terms of the sequence and importance of the transporting forces, aeolian origin is first.
下蜀黄土的成因 ,从营力的先后及主次看 ,风成应是第一位的。
12.
ROCK MAGNETISM OF THE HOLOCENE EOLIAN DEPOSITS IN ?THE LOESS PLATEAU: EVIDENCE FOR PEDOGENESIS
黄土高原全新世风成沉积的岩石磁学性质及其古气候意义
13.
And it is concluded that the aeolian sands and loess are the sediments in the dry-cold period.
风成沙和黄土是晚更新世以来相对干冷气候时期沉积的。
14.
Equivalent dose distribution of aeolian sand using regenerative -dose single-aliquot protocol
沙漠黄土边界带风成沙再生法单片技术等效剂量分布
15.
Comparison of the Sedimentary Features of Loess between the Westerly and Monsoon Regions in China;
中国西风区与季风区黄土沉积特征对比研究
16.
Catchment effect of ridging and mulching in maize field in soil wind erosion area of Loess Plateau
黄土高原土壤风蚀区玉米起垄覆盖集水效应
17.
Influence of Soil Particle Composition on Soil Moisture in Loess Profiles
黄土剖面土壤颗粒组成对土壤含水量的影响
18.
Fractal characteristics of soil particle composition for typical types of soil profile on Loess Plateau
黄土高原典型土壤剖面土壤颗粒组成分形特征