Per Erik Karlsson , Gunilla Pihl Karlsson , Sofie Hellsten , Veronika Kronnäs , Helena Danielsson , Cecilia Akselsson
{"title":"Deposition of phosphorous to open land and forests in Sweden","authors":"Per Erik Karlsson , Gunilla Pihl Karlsson , Sofie Hellsten , Veronika Kronnäs , Helena Danielsson , Cecilia Akselsson","doi":"10.1016/j.aeaoa.2025.100327","DOIUrl":null,"url":null,"abstract":"<div><div>Deposition of phosphorus (P) is important for the nutrient supply to forests and open land but also contributes to the eutrophication of surface waters. Deposition to open land can be measured as bulk deposition while deposition to forests cannot be measured directly, due to internal circulation of P within forest canopies. This study aimed to quantify the total deposition of P to open land and forests in Sweden. The contribution from dry and wet deposition to the deposition to open land was investigated with bulk deposition sampling equipment placed under and outside a roof. The difference with and without the roofs was small and inconsistent. It was concluded that the deposition of P to open land occurred mostly as dry deposition. To estimate the dry deposition of P to coniferous forests, surrogate surfaces consisting of Teflon string samplers were used positioned under roofs. Co-located measurements of dry deposition to forests and bulk deposition to open land at ten different sites across Sweden showed that P deposition was up to five times higher for forests compared to open land. The highest deposition of P to the open land and forests was found for the inland of southern Sweden. This geographical pattern implied only a small contribution from transboundary sources of P outside Sweden. The deposition of P during 2017–2023 was on average 78 g ha<sup>−1</sup> yr<sup>−1</sup> to open land in north and 240 g ha<sup>−1</sup> yr<sup>−1</sup> in inland south Sweden. Corresponding deposition to forests was 120 and 730 g ha<sup>−1</sup> yr<sup>−1</sup>.</div></div>","PeriodicalId":37150,"journal":{"name":"Atmospheric Environment: X","volume":"26 ","pages":"Article 100327"},"PeriodicalIF":3.4000,"publicationDate":"2025-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric Environment: X","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2590162125000176","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Deposition of phosphorus (P) is important for the nutrient supply to forests and open land but also contributes to the eutrophication of surface waters. Deposition to open land can be measured as bulk deposition while deposition to forests cannot be measured directly, due to internal circulation of P within forest canopies. This study aimed to quantify the total deposition of P to open land and forests in Sweden. The contribution from dry and wet deposition to the deposition to open land was investigated with bulk deposition sampling equipment placed under and outside a roof. The difference with and without the roofs was small and inconsistent. It was concluded that the deposition of P to open land occurred mostly as dry deposition. To estimate the dry deposition of P to coniferous forests, surrogate surfaces consisting of Teflon string samplers were used positioned under roofs. Co-located measurements of dry deposition to forests and bulk deposition to open land at ten different sites across Sweden showed that P deposition was up to five times higher for forests compared to open land. The highest deposition of P to the open land and forests was found for the inland of southern Sweden. This geographical pattern implied only a small contribution from transboundary sources of P outside Sweden. The deposition of P during 2017–2023 was on average 78 g ha−1 yr−1 to open land in north and 240 g ha−1 yr−1 in inland south Sweden. Corresponding deposition to forests was 120 and 730 g ha−1 yr−1.
磷(P)的沉积对森林和开阔土地的养分供应很重要,但也有助于地表水的富营养化。对开阔土地的沉积可以作为整体沉积测量,而对森林的沉积不能直接测量,这是由于森林冠层内磷的内部循环。本研究旨在量化瑞典开放土地和森林中磷的总沉积量。通过放置在屋顶下和屋顶外的大块沉积采样设备,研究了干湿沉积对开阔土地沉积的贡献。有屋顶和没有屋顶的差异很小,而且不一致。结果表明,磷在开阔地的沉积以干沉降为主。为了估计磷在针叶林中的干沉降,在屋顶下放置了由特氟龙采样器组成的替代表面。在瑞典10个不同地点对森林的干沉积和开阔土地的大块沉积进行了同步测量,结果表明,森林的磷沉积比开阔土地高5倍。在开阔地和森林中磷的沉积量最高的是瑞典南部内陆。这一地理格局表明,瑞典以外的跨境P来源只占很小的比例。2017-2023年,瑞典北部开阔土地的磷沉降量平均为78 g ha−1 yr−1,南部内陆地区为240 g ha−1 yr−1。相应的森林沉积量分别为120和730 g ha−1 yr−1。