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首页> 外文期刊>European Journal of Soil Science >Soil wetting-drying and water-retention properties in a mine-soil treated with composted and thermally-dried sludges
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Soil wetting-drying and water-retention properties in a mine-soil treated with composted and thermally-dried sludges

机译:用堆肥和热干燥污泥处理过的矿山土壤中的土壤润湿干燥和保水特性

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摘要

The main objective of this study was to analyse how different sewage sludges influence soil wetting and drying dynamics. Three composted and three thermally-dried municipal sludges from different wastewater plants located in Catalonia (NE Spain) were mixed with a mine-soil obtained from a limestone quarry. Measurements of the time required to reach zero contact angle (t(CA) = 0 degrees) and water holding time (WHT) provided information on the time required for a mine-soil to reach its complete wettability and the residence time of water stored between -0.75 and -25 MPa of soil suction, respectively. One month after sludge amendments, one composted and one thermally-dried sludge significantly increased t(CA)= 0 degrees. WHT was increased in the mine-soil treated by composted sludges (50.6% by Blanes' sludge, 65.5% by Manresa's sludge and 52.5% by Vilaseca's sludge) one month after sludge amendments. The amount of water retained in the mine-soil was increased by all composted sludges and one thermally-dried sludge after one month (by 42.3% with Blanes' sludge, 42.3% with Manresa's sludge, 65.7% with Vilaseca's sludge and 23.9% with Mataro's sludge) and one year after sludge amendments and at a small suction. Increments in WHT corresponded with the amount of water retained so the time-scale of soil water availability should also be considered. The t(CA)= 0 degrees. value was modified mainly by increments in carbon stock and microbial biomass, while the WHT was modified mainly by increments in pH and electrical conductivity. Under similar air-drying conditions, mine-soil treated with composted sludges retained more water for longer compared with thermally-dried sludges.
机译:这项研究的主要目的是分析不同的污泥如何影响土壤的湿润和干燥动力学。将来自加泰罗尼亚(西班牙东北部)不同废水处理厂的三种堆肥和三种热干燥的城市污泥与从石灰石采石场获得的矿山土壤混合。测量达到零接触角(t(CA)= 0度)所需的时间和持水时间(WHT),可提供有关矿土达到完全润湿性所需的时间以及所储水之间的停留时间的信息。吸力分别为-0.75和-25 MPa。污泥改良后一个月,一种堆肥和一种热干污泥显着提高了t(CA)= 0度。污泥改良后一个月,经堆肥污泥处理的矿井土壤中的WHT有所提高(Blanes污泥占50.6%,Manresa污泥占65.5%,Vilaseca污泥占52.5%)。一个月后,所有堆肥污泥和一种热干燥污泥增加了矿渣土壤中的水分(Blanes污泥增加了42.3%,Manresa污泥增加了42.3%,Vilaseca污泥增加了65.7%,Mataro污泥增加了23.9%污泥)和污泥修正后的一年,并且吸力很小。 WHT的增加与保留的水量相对应,因此还应考虑土壤水可利用的时间尺度。 t(CA)= 0度。 WHT值主要通过碳储量和微生物生物量的增加来修改,而WHT主要是通过pH值和电导率的增加来修改。在类似的风干条件下,与热干燥污泥相比,用堆肥污泥处理过的矿山土壤保留了更多的水,时间更长。

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