地下水埋深,groundwater depth
1)groundwater depth地下水埋深
1.The characteristics of the soil seed banks follow differentgroundwater depth in the lower reaches of Tarim River;塔里木河下游不同地下水埋深下的土壤种子库特征
2.Spatiotemporal variation of shallowgroundwater depth in intensive agricultural areas;集约化农业生产区浅层地下水埋深的时空变异规律
3.Self-memory model for predictinggroundwater depth series with periodical fluctuation;考虑周期性变化的地下水埋深预测自记忆模型
英文短句/例句
1.The Study on Temporal and Spatial Variation of Groundwater Depth of Western Jilin Province吉林省西部地下水埋深时空变化研究
2.Physiological response of Tamarix spp and Phragmites communis under different groundwater depths不同地下水埋深柽柳、芦苇的生理响应
3.The depth of groundwaterhad fairly greatinfluence to pesticide groundwater contamination.地下水埋深对农药地下水污染的影响颇大。
4.Experiment Research on Reclaimed Water Irrigation under the Conditons of Different Groundwater Depths;不同地下水埋深条件下再生水灌溉的试验研究
5.Variation of Physiological Indexes of the Populus euphraticn" Leaves under Different Groundwater Depth不同地下水埋深下胡杨叶片生理指标变化特点
6.Temporal and spatial variations of groundwater depth in Shiyang River basin石羊河流域地下水埋深时空变化规律研究
7.Influence of Groundwater Depth on Reed"s Budding and Growth地下水埋深对芦苇出苗及苗期生长发育的影响
8.The Response of Shallow Water Table Depths to Climate Change in Huang-Huai-Hai Plain黄淮海平原浅层地下水埋深对气候变化响应
9.Effects of groundwater table on growth characteristics of Alhagi sparsifolia Shap. seedlings骆驼刺幼苗生长特性对不同地下水埋深的响应
10.Physical influencing factors of groundwater depth in Hotan Oasis和田绿洲地下水埋深的自然影响因素分析
11.Study on the Movement and Consumption of SPAC Water in Sandy Artificial Pasture with Shallow Groundwater Table;浅地下水埋深条件下沙质人工草地SPAC水分运移与消耗研究
12.The Utilization Efficiency Experiment and Simulation Evaluation of Soil Water and Fertilizer under Different Groundwater Buried Depth不同地下水埋深下土壤水肥利用效率试验与模拟评价
13.Study on the Impact of Groundwater Depth to Vegetation Ecological Water Requiremengt in Ejina Oasis;地下水埋深对额济纳绿洲植被生态需水量的影响研究
14.Based on ANN model to forecast the groundwater level on the area of well irrigation rice;BP-ANN模型在井灌水稻区地下水埋深预测中的应用
15.Distribution of dominant plant species and characteristic of its communities on the foreland of Cele Oasis in relation to groundwater level策勒绿洲外围不同地下水埋深下主要优势植物的分布和群落特征
16.Study of Ground Water Level Spacial-temperal Dynamic Distribution in Minqin Oasis of Shiyang River Lower Reaches石羊河下游民勤绿洲地下水埋深时空分布动态研究
17.Seasonal variation of groundwater table for Pinus sylvestris var. mongolica plantations in southern Keerqin Sandy land科尔沁沙地南缘樟子松人工林地下水埋深季节变化
18.Spatial distribution of shallow groundwater depth,total dissolved solid and nitrate pollution浅层地下水埋深、矿化度及硝酸盐污染的空间分布特征
相关短句/例句
groundwater table地下水埋深
1.Effects of reclaimed water irrigation on winter wheat growth under differentgroundwater tables;不同地下水埋深条件下再生水灌溉对冬小麦生长的影响
2.Recent advances in desert vegetation response togroundwater table changes;荒漠区植被对地下水埋深响应研究进展
3.Seasonal variation ofgroundwater table for Pinus sylvestris var. mongolica plantations in southern Keerqin Sandy land科尔沁沙地南缘樟子松人工林地下水埋深季节变化
3)groundwater level地下水埋深
1.Distribution of dominant plant species and characteristic of its communities on the foreland of Cele Oasis in relation togroundwater level策勒绿洲外围不同地下水埋深下主要优势植物的分布和群落特征
2.Based on experimental data from laboratory and field experiments, the relationship between rainfall recharge andgroundwater level under farmland drainage is analyzed in this paper.以室内一维土柱试验和室外水平衡小区观测资料为基础 ,对农田排水条件下降雨入渗补给与地下水埋深关系进行了分析 ,根据降雨、蒸发与地下水埋深关系相似的规律 ,仿照国内外排水计算中较为广泛应用的阿维里扬诺夫经验公式的结构形式 ,建立起降雨入渗补给与地下水埋深的关系 ,并采用室内外试验资料对该关系式进行了验证。
3.With special equipments of Central Equipment Station in Shanxi province,this model was established on basis of the results of the optimalgroundwater level range which was measured by taking full advan.为建立新型的节水型灌区,科学用水、计划用水,利用山西省中心试验站蒸渗仪,进行了长达的试验研究,充分利用马氏瓶调控地下水浅埋区的水位动态变化,得出了最佳地下水埋深范围,建立了动态模拟的作物生育期内潜水蒸发模型。
4)groundwater embedment depth地下水埋深
1.In order to solve above-mentioned problems, this paper took 597 Farm as example, built up thegroundwater embedment depth dynamic forecast model of 597 Farm through applying the method of time-series analysis.为了解决上述问题,以597农场为例,采用时间序列分析方法建立了597农场地下水埋深动态预测模型,对地下水埋深进行模拟和预测;同时,揭示了该区地下水动态变化规律,为三江平原地下水资源的可持续利用提供了科学依据。
2.In order to solve above-mentioned problems,this paper took 853 Farm as example,built up thegroundwater embedment depth dynamic forecast model of 853 Farm through applying the method of time-series analysis.为解决上述问题,以853农场为例,采用时间序列分析方法建立了853农场地下水埋深动态预测模型,对地下水埋深进行模拟和预测,揭示了该区地下水动态变化规律,为三江平原地下水资源的可持续利用提供了科学依据。
3.In order to solve above-mentioned problems,this paper took 853 Farm as example,built up thegroundwater embedment depth dynamic prediction model of 853 Farm through applying the method of BP neural network.为解决上述问题,以853农场为例,采用BP神经网络方法建立了853农场地下水埋深动态预测模型,对地下水埋深进行模拟和预测,精度检验结果表明,模型拟合和预测精度均较高。
5)regulation of groundwater depth调控地下水埋深
6)shallow water table地下水浅埋深
1.On the condition ofshallow water table,groundwater,soil moisture,plant water and atmospheric water exchange continuously forming a continuum.通过归纳国内外在地下水浅埋条件下土壤水分运移、土壤盐分运移、以及水盐运移对植物生长发育等生物过程作用的机理等方面的研究成果,综述了近年来国内外在地下水浅埋深条件下GSPAC系统水运移在研究方法、试验和模型方面的进展、各种研究方法的原理、优缺点和今后的研究方向,分析指出定量地研究浅埋深地下水对SPAC系统水分过程、生物过程和能量过程等的作用和影响是一个复合过程,由单个过程研究向过程的综合分析发展难度较大,目前研究相对比较薄弱,是今后需要重点发展的一个方向,在此基础上阐述了GSPAC系统水运移的研究需要深入发展的几个方面。
延伸阅读
地下水水资源评价(见水资源评价)地下水水资源评价(见水资源评价)d ixiashui shuiziyuan Ping】ia地下水水资源评价见水资源评价。
