洛川塬

人为加速侵蚀与自然侵蚀相叠加是近现代洛川塬区沟谷发育、土壤侵蚀剧烈的主要原因。

The main reasons why gully development and soil erosion have been intensifying in Luochuan plateau in modern times are that erosions by personal factors integrate with ones by natural factors .

通过分析得出元代以来洛川塬区沟谷发育速度、土壤侵蚀强度有加剧的趋势，其变化与气候变迁、人类活动关系密切；

By analysis , the paper draws a conclusion that there has been a accelerating tendency in the speed of gully development and the intensity of soil erosion in Luochuan plateau since the Yuan dynasty , which is concerned with climatic variations and human activities .

洛川塬水土流失与黄土构造节理

Soil and Water Loss and Loess Structural Joint in Luochuan Yuan

洛川塬黄土崩塌及水系成因构造因子研究

Study on Structural Factors of Landslides and Origin of Hydrographic Net in Luochuan Loess Plateau

洛川塬区典型农业土壤与苹果园土壤重金属分布调查与评价

Investigation and Assessment on Heavy Metals of Agricultural Soil and Apple Orchard Soil in Luochuan

洛川塬黄土潜水的补给机制及黄土含水特征

The recharge mechanism of unconfined groundwater in the Loess of the Luochuan yuan ~ and its water-bearing characteristics

洛川塬区晚中更新世以来沟谷发育与土壤侵蚀量变化初探

Preliminary Research on Valleys and Gullies Development Process and Quantity of Soil Erosion Changes in Luochuan Loess Plateau Region since Late Middle-Pleistocene

陕北洛川黄土塬是水土流失严重的地区。

Shaanbei Luochuan loess plateau is one of soil erosion districts which is mainly resulted from loess slump .