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Pressurized drainage can effectively reduce subsidence of peatlands - lessons from polder Spengen, the Netherlands

机译:Pressurized drainage can effectively reduce subsidence of peatlands - lessons from polder Spengen, the Netherlands

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Reducing soil subsidence caused by peat oxidation is a major challenge in the Dutch peatlands. To maintain suitable conditions for dairy farming water levels are periodically lowered to keep pace with soil subsidence. Consequently, soil subsidence continues, causing increasing water management costs. We experimented with pressurized drainage in Polder Spengen, a peatland polder in the west of the Netherlands that is primarily used for dairy farming. In this polder, surface water levels of 40 cm below ground surface are maintained, which results in average soil subsidence rates of 7 mmyr~(-1). Pressurized drainage is a novel technique to reduce soil subsidence, it uses field drains that are connected to a small water basin. Surface water can be pumped in or out the water basin, which enables active manipulation of the pressure head in the field drains. The objective of this study is to implement this technique into practice and determine its effect on groundwater tables, soil subsidence rates, and water demand. We applied pressurized drainage in 55 ha of peatland meadows in Polder Spengen, distributed over seven farms. We monitored groundwater tables, surface elevation and water demand. Preliminary results show that during the extreme dry summer of 2018, groundwater tables could be maintained at 40 cm below ground surface, which is 60 cm higher compared to locations without pressurized drainage. This reduced soil subsidence by 50%. Throughout the entire summer of 2018, the water demand amounted to 3-5 mmd~(-1). We believe the technique can effectively contribute to minimize soil subsidence, but relatively high implementation costs may be a barrier to large-scale implementation.
机译:减少泥炭氧化引起的土壤沉降是荷兰泥炭地面临的主要挑战。为了保持奶牛养殖的适宜条件,定期降低水位,以跟上土壤沉降的步伐。因此,土壤继续下沉,导致水资源管理成本增加。我们在荷兰西部试验了泥炭地的排水系统。在该圩区,地表水位保持在地面以下40厘米,导致平均土壤沉降率为7百万年。加压排水是一种减少土壤沉降的新技术,它使用连接到一个小水池的现场排水管。地表水可以泵入或泵出水池,从而能够主动控制油田排水管中的压头。本研究的目的是将该技术付诸实践,并确定其对地下水位、土壤沉降率和需水量的影响。我们在Polder Spengen的55公顷泥炭地草甸中采用加压排水,分布在七个农场。我们监测了地下水位、地表高程和需水量。初步结果显示,在2018年极端干燥的夏季,地下水位可以维持在地表以下40厘米,与没有加压排水的位置相比,地下水位高出60厘米。这减少了50%的土壤沉降。在2018年整个夏季,需水量为3-5 mmd-1。我们认为,该技术可以有效地减少土壤沉降,但相对较高的实施成本可能是大规模实施的障碍。

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