2) piedmont plain
山前平原
1.
Prospective areas and types of aquifer reserve in the Taihang piedmont plain;
太行山前平原地下调蓄远景区与类型
2.
Study on the Calculating Model and Method of Soil Water Resource in Piedmont Plain of Hebei Province;
河北山前平原土壤水资源计算模型与方法研究
3.
This paper divided this region into 4 geomorphological belts:the flood erosion belt,groundwater spill belt,delta belt and the joining belt of piedmont plain and the Tarim floodplain.
将轮台天山南麓山前平原中下部自北至南分为4个地貌带:洪水剥蚀带、溢出带、三角洲带及两河交汇区带。
3) piedmont of Taihang Mountain
太行山山前平原
1.
Analysis of irrigation demands and evapotranspiration in the piedmont of Taihang Mountain;
太行山山前平原区蒸散量和作物灌溉需水量的分析
4) Yanshan piedmont
燕山山前平原
1.
In accordance with the normal,social and economical conditions in Yanshan piedmont,the indictor system was built for a comprehensive benefit evaluation of crop production.
依据燕山山前平原区的自然、社会、经济条件,建立了对该区作物种植生产效益进行综合评价的指标体系,并对目前燕山山前平原区5种主要的作物种植模式进行了效益的综合分析和评价。
5) Taihang Piedmont
太行山前平原
1.
System analysis of typical models of eco-agricultural construction in Taihang Piedmont-A case study from Luancheng County of Hebei Province.;
太行山前平原生态农业建设典型模式系统分析——以河北省栾城县为例
2.
Ways for increasing water use efficiency in farmland of Taihang piedmont.;
太行山前平原农田高效用水模式研究
3.
Kffect of comprehensive water-saving techniques on winter wheat in Taihang Piedmont.;
太行山前平原冬小麦综合节水技术效应分析
6) piedmont plain
山前冲洪积平原
1.
The result of experiments implies that the reserve function of the aquifers from artificial recharge in Taihang piedmont plain of China is related, not only to the reservoir depth of surface water and the time ofwater infiltration but also to the accumulative total volume of water which flows into the reservoir under thecondition of pond infiltration, well injection and channel infiltration.
通过实验研究探讨了太行山前平原地下调蓄能力,实验研究表明,在汇水坑渗、井灌和引水渠渗条件下,太行山前冲洪积平原地下调蓄功能不仅与地表积水深度、入渗时间有关,而且还与汇水总量的多少有关。
2.
The result of experiments implies that the reserve function of the aquifers with river channels from artificial recharge in Taihang piedmont plain of China is related, not only to the accumulative total volume of water and the time of river runoff but also to the unit volume of water which flows throngh rever channels.
实验研究表明 ,在河道过水动水条件下 ,太行山前冲洪积平原地下调蓄功能不仅与总过水量、过水时间有关 ,而且还与河道过水流量的大小有关 ;平均每增加 1个流量 ,引起距河道 95m处地下水位上升 0 。
补充资料：乐山
1.爱好山。
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