1.
THE DISTRIBUTION AND RECLAMATION OF SALINE-ALKALI SOILS OF NORTH CHINA PLAIN AND THE WEI-HO PLAIN IN THE PERIOD OF CHOU-HAN DYNASTIES
周秦两汉时代华北平原与渭河平原盐碱土的分布及利用改良
2.
Tongguan County is located in the transitional region from Shanbei Plateau to Guanzhong Plain, the landform of this county is far from homogenous.
本文重点的研究区域是同官县——一个处于陕北高原向渭河平原过渡地带的县。
3.
The Study on the Evolution of Floods and Water Environment in the West of Guanzhong Plain during the Last Century;
关中平原西部近百年来渭河洪水环境变化研究
4.
Reasons for Constructing the Three Bridges over Weihe River in the Qin and Han Dynasties and the Significance;
秦汉时期渭河三桥的营建原因和重要意义
5.
Optimization Category of Comprehensive Water Use Level in Weihe River Basin
渭河流域综合用水水平的最优化分类研究
6.
Application of Horizontal Directional Drilling Technology in Wei River Crossing
水平定向钻穿越技术在渭河穿越中的应用
7.
Analysis and Evaluation of the Comprehensive Water-using along the Weihe River in Shaanxi Province
陕西省渭河流域综合用水水平分析与评价
8.
RESEARCH ON HORIZONTAL CRUSTAL MOTION AND STRAIN FEATURES OF WEIHE BASIN WITH GPS DATA
渭河盆地现今地壳水平运动及应变特征
9.
Field Water Balance in Dryland of North Weihe and Regulating Technologies;
渭北旱原农田水量平衡及其调控技术研究
10.
Higher-Resolution Studies of the Holocene Pedogenic Environmental Changes on the Fen-Wei Plains;
汾渭平原全新世成壤环境演变的高分辨率研究
11.
Study on the Influence of Polluted Weihe River on Groundwater Through Field Test and Its Numerical Simulation;
渭河污染对地下水影响的原位试验与数值仿真模拟研究
12.
Study on the Penetration Mechanism and the Influence on Groundwater by Pollution of Weihe River Using the Field Test and Numerical Model;
渭河水入渗机理及污染对地下水影响的原位试验及仿真模拟研究
13.
The Meaning of Moderate Seismic Activity Quiet to Strong Earthquakes in Hetao Belt and Fenwei Belt
河套带、汾渭带中等地震活动平静对中强地震的指示意义
14.
Comparative Analysis of Water and Water-Salt Balance of Surface Water and Groundwater in Ogan River Irrigation Area
渭干河灌区地表水与地下水水量及水盐平衡对比分析
15.
Flood Change Research of Weihe River in Wei Nan in Recent 120 Years;
渭南近120年来渭河洪水变化研究
16.
River Ganges Lowland Raw Water Pumping Station
平原河低地原水抽水站
17.
The landform evolution of Xianyang since the end of Qin Dynasty contains two aspects,the northward moving of the Weihe River bed and the changing of the edge slope of Xianyang tableland.
秦末以来,秦都咸阳地貌演变包括渭河河道北移和咸阳原边坡地貌变化两个方面。
18.
A Study on Great Floods Recorded by Sediments on the High Alluvial Flat of Weihe River in Weinan,Shaanxi
渭河渭南段高漫滩沉积记录的洪水研究