机译:土壤水力和气象复杂性对非饱和带时滞估计的影响
Crops, Environment and Land Use Program, Teagasc, Johnstown Castle, Co. Wexford, Ireland,Civil Engineering, National University of Ireland, Galway, Co. Galway, Ireland;
Sustainable Land and Soils, Department for Environment, Food and Rural Affairs, London, United Kingdom;
Crops, Environment and Land Use Program, Teagasc, Johnstown Castle, Co. Wexford, Ireland;
Teagasc Research Operations Group, Statistics and Applied Physics Department, Ashtown, Dublin 15, Ireland;
Civil Engineering, National University of Ireland, Galway, Co. Galway, Ireland;
Earth and Ocean Sciences, National University of Ireland, Galway, Co. Galway, Ireland;
Crops, Environment and Land Use Program, Teagasc, Johnstown Castle, Co. Wexford, Ireland,School of Geosciences, University of the Witwatersrand, Private bag 3, PO Box Wits 2050, Johannesburg, South Africa;
Crops, Environment and Land Use Program, Teagasc, Johnstown Castle, Co. Wexford, Ireland;
Crops, Environment and Land Use Program, Teagasc, Johnstown Castle, Co. Wexford, Ireland;
Time lag; Hydrus; Water quality; Unsaturated;
机译:使用不同土壤质地确定方法进行土壤物理质量和非饱和区时滞估计的后果
机译:检查在不同渗透条件下采集的随时间变化的跨孔GPR数据的信息含量,以估算非饱和土壤水力特性
机译:使用土壤保水数据估算巴西土壤的不饱和水力传导率。
机译:用广义理查兹方程估算非饱和土的水力性质的方法。
机译:从基本的岩土土壤特性估算不饱和压实粘性土壤的水力特性。
机译:根系局部灌溉对玉米土壤-根系水力传导率的影响
机译:不同土壤液压和气象复杂性对不饱和区时间滞后估计的后果
机译:区域5放射性废物管理场地的不饱和区域特征。第1阶段,初步实验室研究,用于测定土壤水分特征曲线和非饱和水力传导率