The objective of this study was to investigate the removal and transformation of dissolved organic matter(DOM) through laboratory-scale soil aquifer treatment(SAT) soil columns.
土壤含水层处理(SAT)对亲水性有机物的去除率为68。
In order to further removal the trihalomethanes precursors in reclaimed water during the secondary effluent reuse,the removal and transformation of dissolved organic matter(DOM) in secondary effluent during the granular activated carbon(GAC) adsorption and the laboratory-scale soil aquifer treatment(SAT) was studied.
为有效控制污水处理厂二级出水在回用水加氯消毒过程中消毒副产物的产生,通过模拟活性炭(GAC)吸附及土壤含水层处理(SAT)实验,研究二级出水经GAC吸附后进行人工地下回灌过程中溶解性有机物(DOM)的迁移及转化规律。
Effect of soil aquifer treatment (SAT)on the secondary treatment effluent was investigated using soil-column experiments.
通过土壤柱实验,研究了土壤含水层处理工艺对污水处理厂二级处理出水的处理效果。
Vegetation temperature condition index(VTCI) drought monitoring approach is applied to monitor droughts and to retrieve surface soil moisture in Junchuan farm of Helongjiang Province in Northeast China.
应用土壤表层含水量数据对干旱监测结果进行验证,验证结果表明VTCI与土壤表层含水量有较好的线性相关性,进一步证实了VTCI是一种实时的干旱监测方法。
Soil moisture condition of Loess Plateau could ensure the positive succession of vegetation although there is a layer of lower soil moisture in natural vegetation that is a normal natural phenomenon.
系统地研究延安研究区的天然植被土壤水分对于认识植被建设的环境具有重要意义,研究结果表明水分条件可以保证植被的正向演替和群落的稳定,虽然在天然植被中也存在土壤低含水层(土壤干层) ,但这是一种正常的自然现象,而且,对植被的自然更新、演替和形成稳定群落没有根本性的影响。
Health Risk Assessment of Reclaimed Wastewater in Soil Aquifer
土壤含水层处理出水的回用健康风险评价
water content of soil
土壤含水量（土壤含水率）
Study on the Soil Moisture Content and Soil Dried Layer under Artificial Forest in Xi an Area;
西安地区人工林土壤含水量与土壤干层研究
Effects of Soil Water Content on Soil Shearing Strength to Different Soil Layer of Shallow Landslide
土壤含水率对浅层滑坡体不同层次土壤抗剪强度的影响
Study on Soil Moisture and Soil Dry Layer in Apple Land and Farmland in Xianyang of Shaanxi Province
陕西咸阳苹果林地和农田土壤含水量及土壤干层研究
after-irrigation moisture content of soil
灌水后土壤中含水量
Spatial variation of saturated hydraulic conductivity and soil water of the surface layer of a slope on the Loess Plateau
黄土高原坡地表层土壤饱和导水率和水分含量空间变异特征
An unconfined aquifer has a water table at its top and water in direct contact with the soil atmosphere.
非承压含水层在它的上面有一个潜水面且水与土壤大气直接相连。
In ABC soil, the uppermost zone of soil, containing humus; topsoil.
淋溶层在ABC层土壤中最上面的一层，含有腐殖土；顶层土壤
Study on Forecast Model of Lower Layers by the Soil Moisture of Surface Layer;
表层土壤水分预测下层土壤水分的模型研究
Research on Methods for Measuring Soil Water Content On-line Based on Digital Image Processing;
基于数字图像处理的土壤表层含水量在线检测方法研究
Study on Retrieval of Soil Moisture Content in Huanghua Using Field Collected Thermal Infrared Data;
基于实测热红外光谱反演黄骅地区表层土壤含水量研究
Influence of Soil Particle Composition on Soil Moisture in Loess Profiles
黄土剖面土壤颗粒组成对土壤含水量的影响
Determination Soil Water Content Using TDR and FDR in the Loess Plateau
TDR和FDR测定黄绵土土壤含水量的标定
Rainfall made soil increase more water if the initial soil water content lower.
土壤初始含水量越低,降雨使土壤水分含量增量越大。
SOIL HYDROLOGIC EFFECT OF THE EARTH-CUMULIC SURFACE HORIZON AND THE ARGIC HORIZON OF LOU SOIL IN LOESS PLATEAU
黄土高原(土娄)覆盖层与黏化层的土壤水文效应
The results showed that the REEs contents in the C horizon the soils were the highest,but Ce was relatively concentrated in A horizon.
结果表明 ,土壤剖面层的底土层含量最高 ,但表土层铈相对富集 .
Chromium(Cr)Level in the Main Topsoil in Henan Province
河南主要土类土壤耕层铬(Cr)含量抽样调查
