Modeling diffuse phosphorus loads from land to freshwater using the sedimentary record

Diffuse: phosphorus (P) loads to a small lake, Friary Lough, in a 1 km(2) a gricultural subcatchment were quantified over 90 years using a palaeolimnol ogical model. The model assumes that lake total phosphorus (TP) is lost to the sediments and to the lake outflow du(r)ing periods of steady-state or i s also stored within the water column during periods of non-steady-state be havior. Reconstructed TP loads during the 1991-1995 time interval of 2.05-2 .53 g m(-2) yr(-1) are verified by hydrochemical monitoring results from th e lake inflow during 1997-1998. This provides evidence for the accuracy of the palaeolomnological model and also that TP loads to the lake dan be acco unted for from external catchment runoff. An analysis of the TP load data i n terms of-catchment exports shows that there was a linear rate of increase from ca. 1946 to 1995 of 1.20- 1.56 kg km(-2) yr(-1). The rate of increase is similar to river P load data in the larger 1480 km(2) catchment tal;en over 17 years, The; rate of TP increase to the lake is interpreted with reg ard to current soil P models that propose increasing and threshold soil P c oncentrations as the cause for increasing diffuse P loss-in runoff.