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1)  uadi ['wædi]
干谷
2)  dry valley
干谷;涸谷
3)  dry valley
干旱河谷
1.
Ecological problems of primary dry valleys is Southwest China and advances in the researches into them;
我国西南主要干旱河谷生态及其研究进展
2.
Differences in growth and reproductive characters of Rosa hugonis in the dry valley of the Upper Minjiang River,Sichuan;
岷江干旱河谷黄蔷薇(Rosa hugonis)生长与繁殖特征及其空间差异
3.
Species diversity and floristic characteristics of woody plants in the dry valley of the Bailong River,China;
白龙江干旱河谷木本植物多样性及其区系地理特征
4)  grain drying
谷物干燥
1.
Infrared-radiative ceramics materials for grain drying;
适用于谷物干燥的红外辐射陶瓷材料
2.
Intelligent real-time on-line measuring system for moisture content during grain drying;
谷物干燥实时在线智能水分测量系统
3.
Energy consumption for grain drying in China;
中国谷物干燥加工中的能源消耗状况(英文)
5)  dry-hot valley
干热河谷
1.
Soil seed bank of vegetation restoration region in mountainous area of Yuanmou dry-hot valley;
元谋干热河谷山地植被修复区土壤种子库研究
2.
Model and effect of ecological restoration of dry-hot valley: A case study of the CAS Dongchuan Debris Flow Observation Station;
干热河谷生态修复模式及其效应——以中国科学院东川泥石流观测研究站为例
3.
Landslide interpretation of remote sensing images in the dry-hot valley of Jinshajiang River;
金沙江干热河谷区滑坡遥感解译研究
6)  dry and hot valley
干热河谷
1.
This article has analyzed conditions of nature geography along dry and hot valley of Jinsha River, elucidated current status in degeneration of ecosystem and put forward technical measurements for guarding against deterioration of ecosystem along dry and hot valley of Jinsha River as well.
本文分析了金沙江干热河谷自然地理条件,阐明其生态系统的退化现状,并提出防止 金沙江干热河谷生态系统恶化的技术措施。
2.
The representative area of dry and hot valley of Jinsha River in Yunnan Province has a temperature condition of the northern tropical zone and a long dry season of more than half a year.
云南金沙江干热河谷典型区具有北热带温度条件和长达半年以上的干季时间,生态系统具有破坏容易恢复难的特点。
3.
Bambusa peruariabilis×Dendro calamopsis daii was introduced from Puwen of Jinghong city to Huaning dry and hot valley in 2000.
2000年从景洪普文镇引入撑绿杂交竹在华宁干热河谷地区引种试验。
补充资料:干谷
干谷
dry valley

   喀斯特区干涸的河谷。又称死谷。底部较平坦,常覆盖有松散堆积物,沿干河床有漏斗、落水洞成群地作串球状分布,往往成为寻找地下河的重要标志。成因很多,中国南方的一些喀斯特谷地,或因地下水位下降、地表水下渗,使原来的喀斯特谷地成为干谷;或因地表曲流段被地下河袭夺,地表留下弯曲的干谷。中国北方喀斯特地区一些河谷,在洪水季节是地表河,在枯水季节则成为干谷。
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