Koichi Kamiya, T. Fukushima, Y. Onda, K. Matsushige, S. Mizugaki
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引用次数: 3
摘要
磷的沉积物-水交换强烈影响湖泊生物地球化学过程和生态系统,特别是在浅湖(例如,WETZEL 2001)。Sebygaard湖是丹麦的一个浅湖,通过比较不同年份不同芯沉积物中TP的垂直剖面来计算总磷(TP)的净释放,尽管外部负荷减少,但内部磷负荷对湖水的影响可以持续30年以上(S0NDERGAARD et al. 1999)。磷随着颗粒物的沉降而沉积(福岛等人,1987年);因此,计算沉积速率和研究沉积物中TP含量在几十年内的垂直剖面变化对确定湖泊磷平衡具有重要意义。本研究分析了日本浅层富营养化湖泊霞aura湖和Suwa湖近30年来沉积物沉积速率和TP含量的变化。基于这些分析,我们比较了TP积累速率估算方法:(1)净负荷;(2) tp含量垂直剖面差异;(3)质量沉降速率乘以TP含量。
Changes in sedimentation rates and phosphorus accumulation in shallow Japanese lakes during 30 years
Sediment-water exchange of phosphorus strongly influences lake biogeochemical processes and ecosystems, especially in shallow lakes ( e.g., WETZEL 2001 ). In Lake Sebygaard, a shallow Danish lake, the net release of total phosphorus (TP) was calculated by comparisons of the vertical pro files of TP in sediments of different cores taken in different years, and influence of interna) phosphorus loads on lake water could last for more than 30 years, despite reduction of externa) loads (S0NDERGAARD et al. 1999). Phosphorus is deposited with sedimentation of particulate matter (FUKUSHIMA et al. 1987); thus, calculation of sedimentation rates and investigation of changes in vertical profiles of TP contents in sediments during severa) decades are important for determining the phosphorus balance in a lake. In this study, we analyzed the changes in sedimentation rates and TP contents in sediment over the 1ast 30 years in Lakes Kasumigaura and Suwa, shallow eutrophic 1akes in Japan. Based on these analyses, we compared TP accumulation rates estimated by: ( 1) net 1oads; (2) difference in vertical profiles ofTP content; and (3) mass sedimentation rates multiplied by TP contents.