黄土地能不能善加利用它的力量创造新机遇？
Can the Yellow Land leverage its power to open up new opportunities?
晚更新世以来自然环境的变化直接影响着黄土高原国土资源的开发利用。
The change of the natural environment of the loess plateau has directly affected the development and utilization of the land resources in the loess plateau.
黄土高原地区水资源缺乏，水资源，特别是土壤水资源的适度开发和合理利用势在必行。
The water resource is short, and rational utilization of water resource, especially soil water resource is imperative on the Loess Plateau.
本研究重点利用GIS辅助土壤侵蚀模型对黄土高原西部的祖厉河流域的土壤侵蚀问题进行了研究。
This research focuses on the erosion problem of ZuLi River basin in the western part of the Chinese Loess Plateau using GIS-assisted soil erosion model.
而且在特定地区(如我国黄土高原地区)，雨水已成为一种不可替代的水资源利用形式。
And in the particular area, such as the Loess Plateau, rainwater has already become a kind of irreplaceable water resources utilization form.
在黄土高原小流域尺度上，地形和土地利用是影响土壤变异的重要因素。
Topography and land use types are key factors which affect soil properties variability on catchment scale in the loess hilly area.
从土地类型数量结构、土地质量结构、土地空间结构和土地利用现状结构入手，对黄土高原沟壑区的土地结构及特征进行了分析。
Based on the land style quality structure, quantity structure, spatial structure and land use structure, the land structure and its characters in the gully area of Loess Plateau were analyzed.
提出了饱和黄土流滑破坏的产生条件和利用稳态强度判断饱和黄土能否产生液化流滑的方法。
Occurrence conditions of liquefaction for loess and the judgment method of flow slide of saturated loess by steady state strength are presented.
黄土髙原沟壑区塬、坡、沟的地貌格局是土地利用空间格局的自然基础。
The plateau-gully-slope morphological pattern of Loess plateau provided a natural foundation of land use structure in the county.
本文介绍一种利用核素示踪技术研究黄土高原不同地形部位土壤侵蚀量的监测新方法。
A new method with nuclear technology to study soil erosion amount monitoring on different topography part in Loess Plateau is reported in this paper.
同时利用工程实测数据，对湿陷性黄土地基上夯锤与土体的共同作用进行了研究。
Moreover, the interaction of the tamper and ground was studied by comparing the calculated values with experimental data obtained on the collapsible loess site.
利用径流冲刷试验，在不同植被格局的坡面上，对黄土丘陵区坡面不同植被格局的侵蚀产沙规律进行了研究。
According to a runoff scouring experiment on different vegetation patterns of slope faces, the loess hilly gully regions different vegetation patterns are studied.
基于中国北方某湿陷性黄土路基工程，利用动力触探和面波法等方法对冲击压实工后的黄土路基进行对比检测。
Based on the collapsible loess subgrade in China northern region, this paper used dynamic sounding method and surface wave method to detect the impact compaction behavior.
本文论述了黄土资源的特性以及利用黄土复垦造地应注意的问题。
This paper discussed the some questions that should be paid attention about the characteristics of loess and its utilization in reclamation.
改善和优化土地利用方式和结构是综合治理黄土高原人为加速侵蚀的关键。
To improve and optimize land use pattern and structure is one of the most effective ways to the control of human-accelerated erosion in the hilly-gully loess region.
利用高速离心机法测试了在不同温度和密度条件下的非饱和黄土的土水特征曲线。
Under different temperature and densities, the soil-water characteristic curves of unsaturated loess were deterrined by centrifuge tests.
利用动三轴实验系统 ，对俄罗斯伊尔库茨克地区黄土的动力特性进行了研究 。
The dynamic characteristics of loess in Irkutsk, Russia are studied by using the dynamic triaxial test.
利用231个气象站多年平均年雨量资料估算了黄土高原地区多年平均降雨侵蚀力，并绘制了等值线图。
Average annual rainfall data from 231 weather stations were used to determine the spatial distribution of erosive rainfall.
现代黄土高原的水土流失是人类长期不合理利用土地资源而加速自然侵蚀的后果。
The soil and water erosion of modern loess plateau is a result that human long-term unreasonable make use of the land resources to accelerate the nature erosion.
二灰黄土是利用石灰、粉煤灰与土料混合作为回填土的一种新型材料，用以代替传统的灰土或素填土。
Lime-fly ash loess, composed of fly ash, lime and loess, is a new material in subgrade backfill to take the place of the (traditional) lime soil.
本课题主要是针对特殊地质的黄土隧洞，利用隧洞衬砌结构计算理论，建立黄土隧洞的衬砌结构计算数学模型。
This subject concerning the loess tunnel which has special geology utilized the tunnel lining structure calculation theory and established the mathematical model of loess tunnel lining structure.
农田爆破成腔技术是黄土区提高天然降水农业利用率的新方法。
The technology of cavity-making by explode in farmland is a new way to improve the agricultural utilization ratio to natural precipitation in the Loess district.
结果表明，陕北黄土高原土壤侵蚀强度和土地利用强度呈高度正相关，说明土地利用强度是导致陕北黄土高原本区域土壤侵蚀的重要驱动力。
The results showed that in this region, soil erosion intensity was highly related to land use intensity, indicating that land use intensity was the main driving force of soil erosion.
利用生物措施中的植被进行黄土高原的水土保持工程与生态环境改良有着明确的目的性与可控制的操作性。
On the basis of which the soil and water conservation engineering and eco-environmental improvement on Loss Plateau by the way of biological means of vegetation will have a clear and decided aim.
黄土高原区可利用能量中用于加热大气的能量占30%，蒸发水分的消耗能量约50%；
In the Loess Plateau, however, only 30% of energy goes to atmosphere heating and 50% is lost to evaporation.
利用GIS技术模拟黄土坡耕地微地形空间分布特征，并对其水土保持效应进行研究。
The spatial distribution of micro-topographical features of loess sloping farmland and its effects of soil and water conservation were studied using GIS under simulated rainfall conditions.
利用GIS技术模拟黄土坡耕地微地形空间分布特征，并对其水土保持效应进行研究。
The spatial distribution of micro-topographical features of loess sloping farmland and its effects of soil and water conservation were studied using GIS under simulated rainfall conditions.
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