School of Biological Sciences, University of Adelaide, Adelaide, SA, Australia.
AgResearch, Lincoln Science Centre, Lincoln, New Zealand; Faculty of Agriculture and Life Sciences, Lincoln University, Lincoln, New Zealand.
Water Res. 2024 Mar 15;252:121201. doi: 10.1016/j.watres.2024.121201. Epub 2024 Jan 30.
The severity and frequency of droughts are projected to increase globally due to climate change, but the effects of this on water quality are uncertain. The Murray-Darling Basin (MDB) is the largest river system in Australia and has been impacted by droughts of varying severity within recent decades. In this study, we assessed the influence of hydrological droughts and their characteristics (severity and duration) on water quality, utilising a long-term (1980-2017) dataset from two monitoring sites. The main drought periods, and their duration and severity, were identified using the calculated Standardised Drought Index values (SDI) from averaged monthly streamflow data. While several hydrological drought periods were identified, the longest duration and greatest severity were during the Millennium Drought (1998-2010). Nutrient loads and concentrations of Total Nitrogen and Total Phosphorus of drought and post-drought periods were significantly different. The drought period showed the lowest median and interquartile range of nutrient (total nitrogen, TN; oxidised nitrogen, NO; total phosphorus, TP; and soluble reactive phosphorus, SRP) concentrations and loads for both sites, whereas the highest nutrient loads and concentrations were reported during the post-drought period (approx. 1 × 10 to 1 × 10 kg day increase in nutrient loads). Our analysis found significant relationships between nutrient loads and SDI during droughts. The load of N and P in the initial flush post-drought increased with drought at both sites. This suggests that nutrients were retained in the landscape during the drought and released in higher loads post-drought when the catchment became wetter, the hydrology was activated, and nutrients were mobilised. Hydrology is a key driver controlling the water quality within the inter-drought period and the peak nutrient loads post-drought. The duration and the severity of droughts had a significant (p = 0.01) influence on peak TN and TP monthly loads but not cumulative loads over a 12-month period. Hydrological droughts are important factors in controlling the water quality of the MDB. Therefore, management efforts should be focused on reducing the occurrence and duration of these events, along with the implementation of catchment nutrient control measures.
由于气候变化,预计全球干旱的严重程度和频率将会增加,但这对水质的影响尚不确定。墨累-达令盆地(MDB)是澳大利亚最大的河流系统,在最近几十年经历了不同严重程度的干旱。在这项研究中,我们利用来自两个监测点的长期(1980-2017 年)数据集,评估了水文干旱及其特征(严重程度和持续时间)对水质的影响。使用从平均每月流量数据计算得出的标准化干旱指数(SDI)值来确定主要干旱期及其持续时间和严重程度。虽然确定了几个水文干旱期,但持续时间最长和最严重的是千年干旱(1998-2010 年)。干旱期和旱后时期的总氮和总磷的养分负荷和浓度有显著差异。干旱期两个站点的养分(总氮,TN;氧化氮,NO;总磷,TP;可溶反应磷,SRP)浓度和负荷中位数和四分位距最低,而旱后时期报告的养分负荷和浓度最高(约增加 1×10 到 1×10 kg day)。我们的分析发现,干旱期间养分负荷与 SDI 之间存在显著关系。在两个站点,旱后初期氮和磷的负荷随着干旱而增加。这表明,在干旱期间,养分被保留在景观中,当集水区变湿时,水文情况被激活,养分被释放,在旱后更高的负荷中释放。水文学是控制旱间期水质和旱后峰值养分负荷的关键驱动因素。干旱的持续时间和严重程度对峰值 TN 和 TP 月负荷有显著影响(p = 0.01),但对 12 个月期间的累积负荷没有影响。水文干旱是控制墨累-达令盆地水质的重要因素。因此,管理工作应侧重于减少这些事件的发生和持续时间,以及实施集水区养分控制措施。