The spatial distribution of groundwater age for different geohydrological situations in the Netherlands: implications for groundwater quality monitoring at the regional scale

被引:56
作者
Broers, HP [1 ]
机构
[1] TNO, Netherlands Inst Appl Geosci, Dutch Geol Survey, NL-3508 TA Utrecht, Netherlands
关键词
groundwater age; tritium; surficial drainage network; heterogeneity; monitoring;
D O I
10.1016/j.jhydrol.2004.04.023
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The spatial distribution of groundwater age is a key factor determining the distribution of dissolved contaminants in the subsurface when contamination loadings have increased in time. The effects of surficial drainage and aquifer heterogeneity on the spatial distribution of groundwater age in unconsolidated aquifers in flat areas were investigated, and consequences were presented for the monitoring of contaminants from diffuse sources. First, the effects were assessed using model simulations. Second, the groundwater age distribution was evaluated in the two regional monitoring networks of Noord-Brabant and Drenthe using tritium measurements. Theoretically, a simple spatial distribution of groundwater age is present in homogeneous aquifers with natural groundwater recharge, characterized by a horizontal pattern of residence time isochrones and a gradual increase of groundwater age with depth. The model simulations show that the isochrone pattern becomes distorted in areas with a surficial drainage network, resulting in relatively old groundwater at shallow depth and larger spatial variation in groundwater age at a specific depth. This drainage effect on the spatial distribution of groundwater age is relatively large compared with effects of regional scale aquifer heterogeneity or spatially varying groundwater recharge. The effects of surficial drainage on the spatial distribution of groundwater age were continued by tritium measurements made in the regional monitoring networks of two provinces in the Netherlands. At about 24 m depth, the proportion of post-1950 groundwater in drained areas was significantly less and the spatial variation of groundwater age was larger than in recharge areas that lack a drainage network. The age of the groundwater appeared to be related to the drainage network density and the water table regime. A preliminary survey showed that contamination patterns in the two networks agree well with the proportion of post-1950 groundwater. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:84 / 106
页数:23
相关论文
共 48 条
[1]  
[Anonymous], THESIS FREE U AMSTER
[2]  
[Anonymous], 1992, STUDIES ENV SCI
[3]  
Bear J., 1988, DYNAMICS FLUIDS PORO
[4]  
Bethke CM, 2002, GEOLOGY, V30, P107, DOI 10.1130/0091-7613(2002)030<0107:POGA>2.0.CO
[5]  
2
[6]   BINOMIAL CONFIDENCE-INTERVALS [J].
BLYTH, CR ;
STILL, HA .
JOURNAL OF THE AMERICAN STATISTICAL ASSOCIATION, 1983, 78 (381) :108-116
[7]  
BROERS HP, 1993, 9393A TNO OS
[8]  
BROERS HP, 1992, H20, V25, P728
[9]  
BROERS HP, 1994, 059438A TNO NOORDBR
[10]  
BROERS HP, 2002, THESIS U UTRECHT