Where do nutrients in an inlet-less lake come from? The water and nutrient balance of a small mesotrophic lake

In this article we verified the hypothesis that precipitation is the main nutrient source in an inlet-less lake. We tested this hypothesis by calculating the water and nutrient (phosphorus and nitrogen) balances of a lake located in a hypsographically diverse moraine landscape (northern Poland). All components of the water and nutrient budgets were measured independently, including precipitation and ground water fluxes. The investigations showed that although precipitation constituted about a half or more of the annual water balance in this inlet-less lake, the ground water inflow and outflow play the most important role in the balance of nutrients. Therefore, critical nutrient loads calculated according to the methodology developed within the OECD Eutrophication Programme, which was focused mostly on drainage-type lakes, appeared inadequate in the case of this small seepage lake. Moreover, studies showed that throughout the investigations, a continuous ground water flow-through occurred in the lake. It questions the possibility of calculating the ground water flow simply as a difference between surface inflows and outflows.