1) Santun River
三屯河
1.
Changes of Santun River and Hutubi River (Xinjiang, China) in the Past 300 Years;
近300年来新疆三屯河与呼图壁河水系变迁研究
2) Santunhe Reservoir
三屯河水库
1.
External Deformation Monitoring and Data Analysis for Santunhe Reservoir Dam in Changji City;
昌吉市三屯河水库大坝外部变形监测及资料分析
2.
Application of TCA in dam external deformation monitoring in Santunhe reservoir;
TCA测量机器人在三屯河水库大坝外部变形监测中的应用
3.
Repair of discharge tunnel in Santunhe Reservoir;
硅粉混凝土在三屯河水库放水隧洞修补中的应用
3) Santunhe channel headq+
三屯河渠道
4) Santunhe irrigation area
三屯河灌区
1.
The large Santunhe irrigation area is an important cotton region in north slope of Tianshan Mountain,where is short of water resource but water waste still exists,although water management and engineering saving water employed.
三屯河灌区属大型灌区,是新疆天山北坡经济带的重要产棉区,灌区水资源短缺,虽然通过加强用水管理和采取工程性节水措施取得了一定的节水成效,但一方面缺水,一方面浪费的局面仍然存在。
5) Santun River basin
三屯河流域
1.
In the paper, In accordance with hydrogeological conditions,groundwater of Santun River basin plain is divided into phreatic water subsystem with single-layer structure,phreatic water both of shallow confined groundwater subsystem and deep confined groundwater subsystem with multi-layer structures.
该文依据水文地质条件将三屯河流域平原区划分为单一结构潜水子系统、多层结构潜水—浅层承压水子系统和深层承压水子系统。
6) Toutunhe Formation
头屯河组
1.
Characteristics of unconformity between the Xishanyao Formation and Toutunhe Formation of Middle Jurassic in Junggar Basin and its significance in petroleum exploration;
准噶尔盆地中侏罗统西山窑组与头屯河组间不整合面特征及其油气勘探意义
2.
Evidence of Existence and Research Significance of Toutunhe Formation in Middle-Che-Mo Palaeo-Uplift within the Central Part of Junggar Basin;
准噶尔盆地腹部车-莫古隆起中段头屯河组存在证据及其研究意义
3.
Application of High Pressure Hg Injection and Rate-controlled Hg Penetration Experimental Technique to Studying Reservoir Microscopic Pore Structure:Taking Toutunhe Formation in Niuquanhu Area of Santanghu Oilfield as an Example;
应用常规压汞和恒速压汞实验方法研究储层微观孔隙结构——以三塘湖油田牛圈湖区头屯河组为例
补充资料：伊春金山屯大丰河漂流
大丰河是汤旺河的一条支流。发源于白山林场163林班，流经白山、丰岭、丰沟、丰源于白山林场经营所，区址南侧1.5公里处注入汤旺河，全长80余公里。两岸沿途大自然风光秀丽，有原始森林、养鹿场、天龙寺等自然、人文景观。
金山屯大丰河漂流的起点位于金山屯区东南部的丰茂林场水泥桥头。漂流河段长1.68万米，水面最大宽度45米，最小宽度l5米；平均宽度为30米,河深1至1.5米，平均流速1米／秒，平均流量3立方米／秒。途中有险滩3处。河床是由细砂和鹅卵石组成。
1994年初夏，金山旅游公司对开发漂流大丰河这一项目进行考察并对沿途进行了整治，疏通了河道。区旅游公司投资一万余元修建了漂游起点码头。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条