Challenges in modelling dissolved organic matter dynamics in agricultural soil using DAISY

被引:49
|
作者
Gjettermann, Birgitte [1 ]
Styczen, Merete [2 ]
Hansen, Hans Christian B. [3 ]
Vinther, Finn P. [4 ]
Hansen, Soren [1 ]
机构
[1] Univ Copenhagen, Dept Agr Sci, Fac Life Sci, DK-2630 Taastrup, Denmark
[2] DHI Water & Environm, Dept Hydrol Soil & Waste, Aarhus, Denmark
[3] Univ Copenhagen, Dept Nat Sci, Fac Life Sci, DK-1168 Copenhagen, Denmark
[4] Univ Aarhus, Inst Agroecol & Environm, Fac Agr Sci, DK-8000 Aarhus C, Denmark
来源
SOIL BIOLOGY & BIOCHEMISTRY | 2008年 / 40卷 / 06期
关键词
dissolved organic matter; dissolved organic C; dissolved organic N; initial mass isotherm; sorption kinetics; organic matter; modelling DOM dynamics; leaching;
D O I
10.1016/j.soilbio.2008.01.005
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Because dissolved organic matter (DOM) plays an important role is terrestrial C-, N- and P-balances and transport of these three components to aquatic environments, there is a need to include it in models. This paper presents the concept of the newly developed DOM modules implemented in the DAISY model with focus on the quantification of DOM sorption/desorption and microbial-driven DOM turnover. The kinetics of DOM sorption/desorption is described by the deviation of the actual DOM concentration in solution from the equilibrium concentration, C-eq. The C-eq is Soil specific and estimated from pedotransfer functions taking into account the soil content of organic matter, Al and Fe oxides. The turnover of several organic matter pools including one DOM pool are described by first-order kinetics. The DOM module was tested at field scale for three soil treatments applied after cultivating grass-clover swards. Suction cups were installed at depths 30, 60 and 90 cm and soil solution was sampled for quantification of dissolved organic C (DOC) and dissolved organic N (DON). In the topsoil, the observed fluctuations in DOC were successfully simulated when the sorption/desorption rate coefficient k was low. In the subsoil, the observed concentrations of DOC were steadier and the best simulations were obtained using a high k. The model shows that DOC and DON concentrations are levelled out in the subsoils due to soil buffering. The steady concentration levels were based on the C-eq for each horizon and the kinetic concept for sorption/desorption of DOC appeared a viable approach. If C-eq was successfully estimated by the pedotransfer function it was possible to simulate the DOC concentration in the subsoil. In spite of difficulties in describing the DOC dynamics of the topsoil, the DOM module simulates the subsoil concentration level of DOC well, and also-but with more uncertainty-the DON concentration level. (C) 2008 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1506 / 1518
页数:13
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