Sökning: "hydraulic conductivity"
Visar resultat 6 - 10 av 57 avhandlingar innehållade orden hydraulic conductivity.
6. Vascular effects of prostacyclin in cat skeletal muscle and in the traumatised rat brain
Sammanfattning : Disturbances in microvascular function may be important for tissue damage in many disease states. Prostacyclin, a substance produced by endothelial cells, is important for the maintenance of normal vascular homeostasis and is a potential drug for treatment of microvascular dysfunction, but indications and optimal dosage remains to be established. LÄS MER
7. Critical hydraulic gradients in tailings dams : comparison to natural analogies
Sammanfattning : The increasing demand of metals and minerals has made it economical for the mining industry to mine low-grade deposits, which results in immense quantities of by-products. In fact, such by-products, i.e. tailings, are the largest waste volumes produced on earth. LÄS MER
8. Climate and geographical influence on the performance of infiltration-based facilities for managing runoff – Temporal and spatial variability
Sammanfattning : Climate change is expected to lead to more intense and severe rainfall events in the future, significantly increasing the risk of urban flooding. This change, characterized by spatial and temporal shifts in precipitation patterns, presents a challenge to the capacity of existing urban drainage systems, which may lead to higher runoff volumes than they were initially designed to handle. LÄS MER
9. Soil Management Strategies to Establish Vegetation and Groundwater Recharge when Restoring Gravel Pits
Sammanfattning : The removal of vegetation and overburden changes the naturalwater purifying processes and thus decreases the groundwaterprotection in gravel pit areas. The sand and gravel depositsusedfor aggregate extraction in Sweden are also often valuablefor extraction of groundwater as a drinking water resource. LÄS MER
10. Multi-Scale Surface Water-Groundwater Interaction : Implications for GroundwaterDischarge Patterns
Sammanfattning : Rivers and aquifers are continuously exchanging water, driven by processes that occur on various temporal and spatial scales, ranging from small streambed features to large geological structures. The interaction between these two components occurs in permeable sediments below the stream channel, called the hyporheic zone. LÄS MER