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区域尺度养分建模:向大堡礁世界遗产区的输出

Regional scale nutrient modelling: exports to the Great Barrier Reef World Heritage Area.

作者信息

McKergow Lucy A, Prosser Ian P, Hughes Andrew O, Brodie Jon

机构信息

Department of Geography, University of Otago, P.O. Box 56, Dunedin, New Zealand.

出版信息

Mar Pollut Bull. 2005;51(1-4):186-99. doi: 10.1016/j.marpolbul.2004.11.030. Epub 2004 Dec 8.

Abstract

Clearing of native vegetation and replacement with cropping and grazing systems has increased nutrient exports to the Great Barrier Reef (GBR) to a level many times the natural rate. We present a technique for modelling nutrient transport, based on material budgets of river systems, and use it to identify the patterns and sources of nutrients exported. The outputs of the model can then be used to help prioritise catchment areas and land uses for management and assess various management options. Hillslope erosion is the largest source of particulate nutrients because of its dominance as a sediment source and the higher nutrient concentrations on surface soils. Dissolved nutrient fractions contribute 30% of total nitrogen and 15% of total phosphorus inputs. Spatial patterns show the elevated dissolved inorganic nitrogen export in the wetter catchments, and the dominance of particulate N and P from soil erosion in coastal areas. This study has identified catchments with high levels of contribution to exports and targeting these should be a priority.

摘要

原生植被的清除以及被种植和放牧系统所取代,已使向大堡礁(GBR)的养分输出增加到自然速率的许多倍。我们提出了一种基于河流系统物质平衡的养分输运建模技术,并利用它来识别输出养分的模式和来源。然后,该模型的输出结果可用于帮助确定集水区和土地利用的管理优先级,并评估各种管理方案。坡面侵蚀是颗粒态养分的最大来源,这是因为它作为沉积物来源占主导地位,且表层土壤中的养分浓度较高。溶解态养分部分占总氮输入的30%和总磷输入的15%。空间格局表明,在较湿润的集水区溶解态无机氮输出量升高,而在沿海地区土壤侵蚀产生的颗粒态氮和磷占主导地位。本研究已确定了对养分输出贡献较大的集水区,将这些集水区作为目标应是当务之急。

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