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Exposure of inner-shelf reefs to nutrient enriched runoff entering the Great Barrier Reef Lagoon: Post-European changes and the design of water quality targets

机译:进入大堡礁礁湖的内层礁石暴露于营养丰富的径流中:后欧洲的变化和水质指标的设计

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We used historical flood plume extent data (modelled) to quantify the typical spatial extent of the summer runoff-seawater mixing zone of the Great Barrier Reef (GBR) lagoon. Spatially explicit analysis of the variability of in situ chlorophyll a concentrations (observed) across the runoff-seawater mixing zone, then allowed us to explore regional differences in the nutrient enrichment impact of runoff events from the various river systems that drain the GBR catchment. We demonstrate the existence of a discernable north-south gradient along the length of the GBR, such that for equivalent runoff:seawater dilutions ratios, lower levels of nutrient enrichment (as indicated by chlorophyll a observations) result from the river systems that drain the relatively undisturbed northern areas of the GBR catchment, compared to more human-impacted central and south areas. We identify a strong correlation between this north-south enrichment gradient and the flood concentration of dissolved inorganic nitrogen (DIN) entrained by the various river systems. By substituting the nutrient enrichment characteristics of the human-impacted river discharges with those of the undisturbed northern rivers, we provide a means to compare the short-term enriching 'footprint' for existing runoff intrusions with those that are likely to have occurred under pre-European catchment conditions. We demonstrate that under pre-European conditions, the nutrient enriching impact from river runoff was likely to have been largely constrained within 1-2 km of the coast, whereas existing conditions support the impact of reefs some 20-30 km off the coast. By using the developed spatial relations, we show that for the heavily human-impacted river systems, reductions in the end-of-river concentrations of DIN in the order 50-80% are needed in order to restore parity with pre-European conditions. We discuss these results in regard to developing end-of-catchment water quality targets for the region.
机译:我们使用历史洪水羽流范围数据(建模)来量化大堡礁(GBR)泻湖夏季径流-海水混合区的典型空间范围。对径流-海水混合区中原位叶绿素a浓度(观察到)的变化进行空间显式分析,然后使我们能够探索排水GBR集水区的各种河流系统的径流事件对养分富集影响的区域差异。我们证明了沿GBR长度存在可辨别的南北坡度,因此,对于等效的径流:海水稀释比,较低的养分富集水平(如叶绿素a的观察结果)是由相对较高的排水系统引起的。与受人为影响更大的中部和南部地区相比,GBR流域的北部地区不受干扰。我们确定了这种南北富集梯度与各种河流系统夹带的溶解性无机氮(DIN)的洪水浓度之间的强烈相关性。通过用人为影响的河流排放物的养分富集特征代替未受干扰的北部河流的养分富集特征,我们提供了一种方法,可以比较现有径流入侵的短期富集“足迹”与在径流前可能发生的入侵。欧洲集水条件。我们证明,在欧洲之前的条件下,来自河流径流的养分富集影响可能很大程度上被限制在海岸的1-2公里之内,而现有条件支持了离海岸约20-30公里的礁石的影响。通过使用已开发的空间关系,我们表明,对于受人类影响严重的河流系统,需要将河流末端的DIN浓度降低50-80%左右,以恢复与欧洲前时期的状况一致。我们讨论了有关为该地区制定集水区终端水质目标的这些结果。

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