首页 | 本学科首页   官方微博 | 高级检索  
   检索      


Benthic shear stress gradient defines three mutually exclusive modes of non-biological internal nutrient loading in shallow lakes
Authors:Daniel B Thomas  Marc Schallenberg
Institution:(1) Department of Zoology, University of Otago, P.O. Box 56, Dunedin, 9054, New Zealand;(2) Present address: Geology Department, University of Otago, P.O. Box 56, Dunedin, 9054, New Zealand
Abstract:Assessment of the importance of internal nutrient loading is essential for managing and restoring eutrophic shallow lakes. To date, studies of internal loads have tended to focus on one of two abiotic processes, either molecular diffusion or sediment/nutrient entrainment (resuspension). This study presents a new approach to determining the non-biological fluxes of nitrogen (N) and phosphorus (P) from the sediment to the water column of shallow lakes. Three mutually exclusive flux processes: (i) molecular diffusion, (ii) turbulent diffusion (eddy diffusivity) and (iii) wind-induced resuspension of N and P, were related to a gradient of benthic shear stress. A model presented here allowed the durations and magnitudes of different non-biological fluxes to be calculated over time, based on benthic shear stress. Two site-specific critical shear stress thresholds determined which of the three flux processes dominated for any benthic shear stress value. The model was calibrated for a shallow lake and the continuous flux of nutrient from the sediment to the overlying water generated by each process during that period was calculated, enabling the estimation of the relative importance of each of the three flux processes over a one-year period. Wind-induced resuspension dominated the internal nutrient flux, operating for 38% of the time and contributing 0.9 T P year−1 and 10.2 T N year−1 to the internal nutrient load. In contrast, molecular diffusion only contributed 0.01–0.02 T P year−1 and 0.12–0.20 T N year−1 to the water column, while turbulent diffusion provided up to 0.6 T P year−1 and 6.2 T N year−1. Our model suggests that turbulent diffusion is a neglected and potentially important process contributing to internal nutrient loading in shallow lakes, whereas molecular diffusion appears to be relatively unimportant in lakes that experience turbulence at the sediment–water interface. Handling editor: L. Naselli-Flores
Keywords:Flux  Diffusion  Molecular  Turbulence  Resuspension  Eutrophication  Restoration  Internal loading  Nutrient  Nitrogen  Phosphorus  Model  Lake Waihola  Shallow lake
本文献已被 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号