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1)  annual balanced underground water level or setting depth
年平衡地下水位或埋深
2)  groundwater depth
地下水位埋深
1.
Based on the ecological fitting theory,the thesis systematically analyzed the quantitative relationship between plant ecotype and groundwater depth as well as soil water content,according to the test data in sample area and the plant ecotypes in Horqin sandy land.
水分是干旱区植物生长的限制因子,以生态适宜性理论为基础,根据科尔沁沙地植被生态型及典型样带调查试验资料,系统分析了植物生态型与地下水位埋深及土壤含水率的定量关系。
2.
Based on the remote sensing data,surface soil salt and groundwater table data,this paper studied the relationships between the soil salinization and the vegetation,groundwater depth in Yinchuan plain.
结果表明:随着表层土壤含盐量的增大,NDVI(归一化植被指数)逐渐减小,植被发育较好的区域土壤含盐量均小于3 g/kg;植被主要生长在没有盐渍化或轻微盐渍化的地区,在中度和重度盐渍化地区几乎没有植被发育;在枯水季节,研究区土壤盐渍化最严重的地下水位埋深为1。
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 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
2.
Based on experimental data from laboratory and field experiments, the relationship between rainfall recharge and groundwater 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 optimal groundwater 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10年的试验研究,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 table
地下水埋深
1.
Effects of reclaimed water irrigation on winter wheat growth under different groundwater 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 to groundwater table changes;
荒漠区植被对地下水埋深响应研究进展
3.
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
5)  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 the groundwater 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 the groundwater 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 the groundwater 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。
6)  groundwater depth
地下水埋深
1.
The characteristics of the soil seed banks follow different groundwater 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 shallow groundwater 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 predicting groundwater 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
补充资料:怀深法师(1076~1132年)
【怀深法师(1076~1132年)】
  慈受怀深和尚,安徽人,俗姓夏。十八岁游方,二十六岁到福建资圣寺,依于长芦崇信。三十七岁请住城南资福寺,学徒云集。乡民迷信,建土地祠于寺内,以致杂秽,怀深遣去院外,作偈云:‘村歌社舞拜祠堂,臭秽腥膻污道场;要答神明冥护力,晨昏烧取一炉香。’
  平时持律清严,用心于训童,其行颂之一云:‘莫说他人短与长,说来说去自招殃;若能闭口深藏舌。便是修身第一方。’蒋山佛鉴,渡江行化到资福,巡寮到千人街坊。鉴:‘既是千人街坊,为什么只有一人?’深:‘多虚不如少实。’鉴:‘恁么耶?’怀深赫然。四十一岁离资福,到蒋山请益于佛鉴,鉴:‘资福知是般事便休。’深:‘其实未稳,望和尚不外。’鉴与倩女离魂话,反复究之,怀深于此,透脱疑碍,呈偈云:‘只是旧时行李处,等闲举著便淆讹;夜来一阵狂风起。吹落桃华知几多。’鉴喜曰:‘这底,岂不是活祖师意?’敕住焦山禅寺四年,四十五岁敕住东京慧林禅院,五十岁辞退,上天台,移住灵岩,敕补蒋山。退居洞庭包山,住显尘庵,作洞庭十二偈,拟寒山诗二十首,退步偈十二首,其中一首云:“万事无如退步人,孤云野鹤自由身;松风十里时来往,笑揖峰头月一轮。”请住江西思溪圆觉寺为第一祖。五十八岁为众小参,有僧问末后句,深:‘后五日看。’果然,经五日,微疾而化。
  (曾普信 著)(根据网上资料编辑)
  
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