| 1. | Soil quality - determination of the water - retention characteristic - laboratory methods
土壤质量.水保持特性的测定.实验室法 |
| 2. | Soil quality - determination of the water retention characteristics - laboratory methods iso 11274 : 1998
土壤质量.水分保持特性的测定.实验室法 |
| 3. | Soil quality - determination of unsaturated hydraulic conductivity and water retention characteristic - wind ' s evaporation method
土质.非饱和水渗导性和水保持特性的测定.风蒸发法 |
| 4. | Soil quality - determination of unsaturated hydraulic conductivity and water - retention characteristic - wind ' s evaporation method
土质.非饱和水渗导性和水保持特性的测定.风的蒸发法 |
| 5. | Soil quality - determination of unsaturated hydraulic conductivity and water - retention characteristic - wind ' s evaporation method iso 11275 : 2004
土质.非饱和水渗导性和水分保持特性的测定.风蒸发法 |
| 6. | Standard test method for retention characteristics of 0 . 2 - 181m membrane filters used in routine filtration procedures for the evaluation of microbiological water quality
评定微生物水质的常规过滤程序用0 . 2微米薄膜过滤器滞留特性的标准试验方法 |
| 7. | Standard test method for retention characteristics of 0 . 40 to 0 . 45 - 181m membrane filters used in routine filtration procedures for the evaluation of microbiological water quality
评定微生物水质的常规过滤程序用0 . 4微米到0 . 45微米薄膜过滤器滞留特性的标准试验方法 |
| 8. | The relationship of soil particle - size distributions and soil water retention characteristics , saturated and unsaturated hydraulic conductivity were studied in the lab
本研究对陕西四种不同质地土壤的粒径分布与水分特征曲线及饱和、非饱和导水率的关系进行了研究。 |
| 9. | It can be use as a parameter to describe the variety of soil texture . 3 . on the basis of the a & p model , soil particle - size distributions and soil bulk density data is translated to soil water retention characteristics
A & p模型得出的四种土壤的水分特征曲线，在低吸力范围段可以较好反映土壤实际的土水势与含水量之间的关系。 |
| 10. | In low matric potential state , the a & p model can be use to predict water retention characteristics , but in high matric potential state , it cannot get good result . in addition of soil pore connectivity , to correct the a & p model , it can get good result in whole water content range
但在高吸力段a & p模型预测的结果与实际偏差较大，考虑到土壤孔隙实际联通状况，修正a & p模型，使供试的四种在整个含水量范围对土壤水分特征曲线都得到了较好的拟合。 |
