Assessment of phosphorus behavior in sediments of Lake Sevan, Armenia

Pub Date : 2023-10-25 DOI:10.4081/jlimnol.2022.2132
T. Dadi, Wolf Von Tümpling, Chenxi Mi, Martin Schultze, Kurt Friese
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Abstract

Lake Sevan is the largest freshwater lake in the Caucasus region and one of Eurasia's largest alpine lakes. The lake has been experiencing growing cyanobacteria blooms; however, the relevance of external and internal phosphorus (P) loading to its eutrophication is still not known. We carried out a sediment investigation of Lake Sevan to estimate the potentially mobile P, which could be a source of internal total phosphorus (TP)-loading; we also estimated external TP-loading and retention. The study was carried out at four sampling points of different depths to determine the spatial variability of P in 2018. The sediments had elevated TP contents at the sediment surface; potentially mobile P ranged from 20 to 60% in the top 2 cm. The upper 4 cm sediment had an elevated content of TN (8 to 16.1 mg N g-1 dw) and TP (1.2 to 1.7 mg P g-1 dw). Spatial variability of most of the measured parameters was more prominent in the upper 3 cm. External TP loading was estimated to be 110 tons annually, and the TP retention was 85%. The estimated TP stored in the top cm of the sediment is 1,500 tons. The potential for P release is high; the short-term exchange between oxic and anoxic overlying water could release 0.01 to 0.02 mg P L-1 from the top cm of the sediment, and long-term diagenesis and burial could release about 0.12 mg P cm-2. Internal P-loading in Lake Sevan may play an essential role in eutrophication, especially given the long flushing time of Lake Sevan.
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亚美尼亚塞万湖沉积物中磷行为评估
塞万湖是高加索地区最大的淡水湖,也是欧亚大陆最大的高山湖泊之一。该湖的蓝藻水华日益严重;然而,外部和内部磷(P)负荷对其富营养化的影响尚不清楚。我们对塞万湖的沉积物进行了调查,以估算可能成为内部总磷 (TP) 负荷来源的潜在移动磷;我们还估算了外部 TP 负荷和滞留情况。研究在四个不同深度的取样点进行,以确定 2018 年 P 的空间变化。沉积物表面的 TP 含量较高;顶部 2 厘米处的潜在可移动 P 含量介于 20% 到 60% 之间。上部 4 厘米沉积物的 TN(8 至 16.1 毫克 N 克-1 干重)和 TP(1.2 至 1.7 毫克 P 克-1 干重)含量升高。大部分测量参数的空间变异性在上 3 厘米处更为突出。外部 TP 负荷估计为每年 110 吨,TP 保留率为 85%。据估计,沉积物最上层厘米的 TP 储量为 1,500 吨。P 释放的潜力很大;上覆含氧水和缺氧水之间的短期交换可从沉积物顶部厘米释放 0.01 至 0.02 毫克 P L-1,长期成岩作用和埋藏可释放约 0.12 毫克 P cm-2。塞万湖的内部 P 负荷可能在富营养化过程中发挥了重要作用,特别是考虑到塞万湖的冲刷时间较长。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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