Stenemo Fredrik, Jørgensen Peter R, Jarvis Nicholas
Department of Soil Sciences, SLU, Box 7014, 750 07 Uppsala, Sweden.
J Contam Hydrol. 2005 Sep;79(1-2):89-106. doi: 10.1016/j.jconhyd.2005.06.004.
The one-dimensional pesticide fate model MACRO was loose-linked to the three-dimensional discrete fracture/matrix diffusion model FRAC3DVS to describe transport of the pesticide mecoprop in a fractured moraine till and local sand aquifer (5-5.5 m depth) overlying a regional limestone aquifer (16 m depth) at Havdrup, Denmark. Alternative approaches to describe the upper boundary in the groundwater model were examined. Field-scale simulations were run to compare a uniform upper boundary condition with a spatially variable upper boundary derived from Monte-Carlo simulations with MACRO. Plot-scale simulations were run to investigate the influence of the temporal resolution of the upper boundary conditions for fluxes in the groundwater model and the effects of different assumptions concerning the macropore/fracture connectivity between the two models. The influence of within-field variability of leaching on simulated mecoprop concentrations in the local aquifer was relatively small. A fully transient simulation with FRAC3DVS gave 20 times larger leaching to the regional aquifer compared to the case with steady-state water flow, assuming full connectivity with respect to macropores/fractures across the boundary between the two models. For fully transient simulations 'disconnecting' the macropores/fractures at the interface between the two models reduced leaching by a factor 24. A fully connected, transient simulation with FRAC3DVS, with spatially uniform upper boundary fluxes derived from a MACRO simulation with 'effective' parameters is therefore recommended for assessing leaching risks to the regional aquifer, at this, and similar sites.
一维农药归趋模型MACRO与三维离散裂隙/基质扩散模型FRAC3DVS松散耦合,用于描述丹麦哈夫德鲁普一处冰碛土和局部砂质含水层(深度5 - 5.5米)中农药麦草畏的运移情况,该局部含水层位于区域石灰岩含水层(深度16米)之上。研究了地下水模型中描述上边界的替代方法。进行了场尺度模拟,以比较均匀上边界条件与基于MACRO的蒙特卡罗模拟得出的空间可变上边界。进行了地块尺度模拟,以研究地下水模型中通量上边界条件的时间分辨率的影响,以及两个模型之间关于大孔隙/裂隙连通性的不同假设的影响。田间淋溶变异性对局部含水层中模拟的麦草畏浓度的影响相对较小。假设两个模型之间的边界处大孔隙/裂隙完全连通,与稳态水流情况相比,FRAC3DVS的全瞬态模拟得出进入区域含水层的淋溶量要大20倍。对于全瞬态模拟,“断开”两个模型界面处的大孔隙/裂隙会使淋溶量减少24倍。因此,对于评估该场地及类似场地对区域含水层的淋溶风险,建议采用FRAC3DVS进行全连通、瞬态模拟,并采用基于“有效”参数的MACRO模拟得出的空间均匀上边界通量。