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瑞典农业用地磷素流失减缓措施的批判性评估

Critical evaluation of measures to mitigate phosphorus losses from agricultural land to surface waters in Sweden.

作者信息

Ulén B, Jakobsson C

机构信息

Division of Water Management, Department of Soil Sciences, Swedish University of Agricultural Sciences, Box 7014, SE-750 07 Uppsala, Sweden.

出版信息

Sci Total Environ. 2005 May 15;344(1-3):37-50. doi: 10.1016/j.scitotenv.2005.02.004. Epub 2005 Apr 7.

DOI:10.1016/j.scitotenv.2005.02.004
PMID:15907509
Abstract

The aim of this paper is to collate information on potential measures to reduce phosphorus (P) losses, with particular reference to Sweden. In Sweden, three dominant types of soils or soil profiles are at risk of suffering from high P losses through different pathways: clay soils with a naturally poor structure, usually situated on the large central plains, are prone to lose P through drain tiles; silty soils, usually situated on hilly terrain, are prone to erosion; and sandy soils with a low P sorption capacity in both topsoil and subsoil and that have had heavy applications of fertilisers, are prone to high leaching losses. Fields with such soils and landscape position with connectivity to surface waters may lose more than 0.5 kg P ha year-1 and often more than 1 kg P ha year-1. Losses of soluble reactive P (SRP) are commonly 30-50% of the total P losses. Improved soil tillage together with other measures aimed at improving soil structure are suggested to have the best potential to reduce losses, with short-term and long-term effects, for the clayey and silty soil profiles. For the silty soils, keeping the surface densely vegetated in winter and liming backfill of the drainage systems are suggested to be important ways to reduce the losses of particulate P (PartP). For sandy soils prone to P leaching, appropriate application of fertiliser and improved contact between fertiliser and the soil may be one of the few effective ways to reduce SRP losses.

摘要

本文旨在整理有关减少磷(P)流失的潜在措施的信息,特别以瑞典为例。在瑞典,有三种主要类型的土壤或土壤剖面存在通过不同途径遭受高磷流失的风险:结构天然较差的黏土,通常位于中部大平原,容易通过排水瓦管流失磷;粉质土,通常位于丘陵地带,容易遭受侵蚀;表土和底土对磷吸附能力低且大量施用化肥的砂土,容易出现高淋失量。具有此类土壤且与地表水有连通性的田地每年可能流失超过0.5千克磷/公顷,且通常超过1千克磷/公顷。可溶性活性磷(SRP)的流失通常占总磷流失量的30%-50%。对于黏质土和粉质土剖面,建议改良土壤耕作并结合其他旨在改善土壤结构的措施,这在减少流失方面具有最佳潜力,且具有短期和长期效果。对于粉质土,建议在冬季保持地表植被茂密以及对排水系统进行石灰回填,这是减少颗粒态磷(PartP)流失的重要方法。对于容易发生磷淋失的砂土,合理施用化肥并改善化肥与土壤之间的接触可能是减少SRP流失的少数有效方法之一。

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