Southern Cross Geoscience, Faculty of Science and Engineering, Southern Cross University, Lismore, NSW 2480, Australia.
Southern Cross Geoscience, Faculty of Science and Engineering, Southern Cross University, Lismore, NSW 2480, Australia.
Water Res. 2022 Jun 30;218:118510. doi: 10.1016/j.watres.2022.118510. Epub 2022 Apr 25.
Increased frequency and intensity of drought, wildfires and flooding due to climate change has major implications for river water quality, yet there are limited high-temporal resolution data capturing the combined transient impacts of these extreme events at large catchment scales. We present flow-stratified water quality data from a large coastal catchment (Macleay River, Australia) spanning severe drought and extensive fires followed by flooding. We examine concentrations (C), discharge (Q) and flux of suspended sediment, major ions, dissolved organic carbon (DOC) and key nutrients (NO and PO), with a focus on the critical first-flush period after the fires. Highly elevated suspended sediment (∼5500 mg L; >100x median pre-fire levels) during the initial post-fire period reflected enhanced erosion from fire-impacted, high-relief landscapes, with peak monthly suspended sediment loads of ∼1.1-3.7 t ha. The greatest sensitivity to erosion was during initial flow events following fire, highlighting the compounding effect of sequential extreme events on sediment transport. Maximum solute concentrations typically occurred during the first hydrograph peak post-fire with significantly (P = 0.01) elevated major ions following the order of K>Ca>SO>HCO≈Mg>Cl>Na, broadly reflecting the composition of ash materials. Distorted CQ relationships for major ions, DOC and nutrients indicated mobilisation behaviour and enhanced surface runoff during initial hydrograph peaks post-fire, with mean concentrations and CQ relationships progressively shifting to those approximating pre-fire within ∼3-12 months. Elevated DOC (∼7x; P = 0.01) displays distinct changes in fluorescence excitation-emission matrix spectral characteristics, attributable to both fire and drought. Both NON (160 μM) and PO (7.5 μM) were significantly elevated after the fires (∼15-22x; P = 0.01), with maximum monthly loads of 0.82 and 0.14 kg ha respectively. Fast biogeochemical cycling of dissolved inorganic nitrogen (DIN) species occurred during initial flow events following fire, with NHN initially dominant (>80% of DIN) and exceeding ecosystem guideline threshold values (>100 μM NHN), followed by rapid (∼1 week) nitrification. The extreme dynamism and transience of water quality parameters highlights the critical importance of high-frequency sampling to adequately capture the compound impacts drought, fires and floods on aquatic systems.
由于气候变化,干旱、野火和洪水的频率和强度增加,这对河流水质有重大影响,但在大型集水区范围内,能够同时捕捉到这些极端事件的综合瞬时影响的高时间分辨率数据十分有限。我们提供了一个大型沿海流域(澳大利亚的麦考利河)在严重干旱和广泛野火之后发生洪水的水文分层水质数据。我们检测了悬浮泥沙、主要离子、溶解有机碳(DOC)和关键养分(硝氮和磷)的浓度(C)、流量(Q)和通量,重点关注火灾后的首个洪水峰期。在最初的火灾后时期,由于受火灾影响的高起伏景观增强了侵蚀作用,导致悬浮泥沙高度升高(约 5500 mg/L;是火灾前水平的 100 倍以上),每月悬浮泥沙负荷的峰值达到 1.1-3.7 t/ha。在火灾后最初的水流事件中,对侵蚀的敏感性最大,突出了连续极端事件对泥沙输移的复合影响。最大的溶质浓度通常出现在火灾后首个洪水峰期,主要离子的浓度显著升高(P=0.01),顺序为 K>Ca>SO>HCO≈Mg>Cl>Na,大致反映了灰分物质的组成。主要离子、DOC 和养分的 QC 关系扭曲,表明在火灾后最初的洪水峰期,物质的迁移行为和地表径流量增加,平均浓度和 QC 关系在大约 3-12 个月内逐渐转变为接近火灾前的状态。DOC (约 7 倍;P=0.01)的荧光激发-发射矩阵光谱特征发生了明显变化,这归因于火灾和干旱的共同作用。氮(NON)和磷(PO)在火灾后显著升高(约 15-22 倍;P=0.01),最大月负荷分别为 0.82 和 0.14 kg/ha。在火灾后最初的水流事件中,溶解无机氮(DIN)物种发生了快速的生物地球化学循环,NHN 最初占主导地位(>DIN 的 80%),并超过生态系统指南阈值(>100 μM NHN),随后迅速(约 1 周)硝化。水质参数的极端动态和瞬态变化突出表明,高频采样对于充分捕捉干旱、火灾和洪水对水生系统的综合影响至关重要。