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1)  Luohuiqu irrigation district
洛惠渠灌区
1.
Simulation study on groundwater level dynamic in Luohuiqu irrigation district
洛惠渠灌区地下水位动态模拟研究
2.
In order to deeply seek the variation of groundwater dynamic, groundwater dynamic under natural-artificial-biological conditions was studied with measured data of Luohuiqu irrigation district in Shaanxi as an example based on the application of BP network of three layers.
为了深入探求地下水动态变化规律,以陕西洛惠渠灌区多年实测数据为例,首先引用3层前馈型BP网络建模方法,对灌区自然-人工-生物条件下地下水动态进行了研究,其次采用改进的灰色斜率关联度方法分析了各影响因子与地下水埋深的敏感程度,根据斜率关联度进行了综合排序。
2)  East main canal of Luohui Irrigation district
洛惠渠灌区东干渠
3)  Luo-hui irrigation scheme
洛惠灌区
4)  Jinghuiqu irrigation district
泾惠渠灌区
1.
Impact of Climate and Discharge Change on Sustainable Development in Jinghuiqu Irrigation District and Countermeasures
气候与径流变化对泾惠渠灌区可持续发展的影响与对策研究
2.
Jinghuiqu Irrigation District are locats in the central of the Guanzhong plain.
泾惠渠灌区地处关中平原中部,是一个引泾河水自流灌溉的大型灌区。
5)  Jinghuiqu Irrigation Area
泾惠渠灌区
1.
Jinghuiqu Irrigation Area is located in the centre of Guanzhong Plain, where the groundwater is the main water sources of irrigation and water supply.
泾惠渠灌区地处关中平原中部,地下水是该灌区重要的灌溉和供水水源。
2.
Western Suburbs Reservoir is an internal reservoir of JingHuiQu irrigation area, using the terrain of the Loess Plateau ravine, which has been built and run in 2003.
在泾惠渠灌区现有的调配方案与工程现状基础上,为使灌区获得最大的灌水量,通过分析计算渠首引水量、灌区需水量、渠系灌溉的余水弃水量、西郊水库的引水量等资料,建立以灌区灌溉缺水量最小为目标的优化模型,应用遗传算法,对西郊水库进行模拟调节计算。
3.
In order to study the regulation of time-domain variation of soil moisture in the semi-arid areas,the testing of soil moisture content on different time in Jinghuiqu irrigation area was conducted introduced TRIME-TDR Soil Moisture Testing Equipment for three different irrigation quotas.
为了研究半干旱区土壤水分时空变化规律,针对三种不同的灌溉定额,采用TRIME-TDR土壤水分测试仪对渭北平原的泾惠渠灌区土壤水分进行不同时刻的测定,通过对同一时刻不同灌溉量对土壤水分的影响以及同一灌溉量对土壤水分随时间变化的影响研究,得出了灌区土壤水分下渗的基本规律以及灌区的最佳灌溉定额为2。
6)  Longdong-Jinghuiqu Iirrgation Area
龙洞-泾惠渠灌区
补充资料:九日洛东亭
【诗文】:
风息斜阳尽,游人曲落间。采花因覆酒,行草转看山。
柳散新霜下,天晴早雁还。伤秋非骑省,玄发白成斑。



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【出处】:
全唐诗:卷293_51
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