Response to recharge variation of thin rainwater lenses and their mixing zone with underlying saline groundwater

被引:17
作者
Eeman, S. [1 ]
van der Zee, S. E. A. T. M. [1 ]
Leijnse, A. [1 ]
de Louw, P. G. B. [2 ]
Maas, C. [3 ]
机构
[1] Wageningen Univ, Environm Sci Grp, NL-6700 AA Wageningen, Netherlands
[2] Deltares, Dept Soil & Groundwater, NL-3508 AL Utrecht, Netherlands
[3] KWR Watercycle Res Inst, NL-3430 BB Nieuwegein, Netherlands
关键词
SEA-LEVEL RISE; CLIMATE-CHANGE; COASTAL AQUIFER; WATER INTERFACE; FRESH; TRANSPORT; DISPERSION; DISCHARGE; SURFACE; REGION;
D O I
10.5194/hess-16-3535-2012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In coastal zones with saline groundwater, fresh groundwater lenses may form due to infiltration of rain water. The thickness of both the lens and the mixing zone, determines fresh water availability for plant growth. Due to recharge variation, the thickness of the lens and the mixing zone are not constant, which may adversely affect agricultural and natural vegetation if saline water reaches the root zone during the growing season. In this paper, we study the response of thin lenses and their mixing zone to variation of recharge. The recharge is varied using sinusoids with a range of amplitudes and frequencies. We vary lens characteristics by varying the Rayleigh number and Mass flux ratio of saline and fresh water, as these dominantly influence the thickness of thin lenses and their mixing zone. Numerical results show a linear relation between the normalised lens volume and the main lens and recharge characteristics, enabling an empirical approximation of the variation of lens thickness. Increase of the recharge amplitude causes increase and the increase of recharge frequency causes a decrease in the variation of lens thickness. The average lens thickness is not significantly influenced by these variations in recharge, contrary to the mixing zone thickness. The mixing zone thickness is compared to that of a Fickian mixing regime. A simple relation between the travelled distance of the centre of the mixing zone position due to variations in recharge and the mixing zone thickness is shown to be valid for both a sinusoidal recharge variation and actual records of daily recharge data. Starting from a step response function, convolution can be used to determine the effect of variable recharge in time. For a sinusoidal curve, we can determine delay of lens movement compared to the recharge curve as well as the lens amplitude, derived from the convolution integral. Together the proposed equations provide us with a first order approximation of lens characteristics using basic lens and recharge parameters without the use of numerical models. This enables the assessment of the vulnerability of any thin fresh water lens on saline, upward seeping groundwater to salinity stress in the root zone.
引用
收藏
页码:3535 / 3549
页数:15
相关论文
共 49 条
[1]   Anisotropic dispersive Henry problem [J].
Abarca, Elena ;
Carrera, Jesus ;
Sanchez-Vila, Xavier ;
Dentz, Marco .
ADVANCES IN WATER RESOURCES, 2007, 30 (04) :913-926
[2]   Transport modeling of nonlinearly adsorbing solutes in physically heterogeneous pore networks [J].
Acharya, RC ;
Van der Zee, SEATM ;
Leijnse, A .
WATER RESOURCES RESEARCH, 2005, 41 (02) :1-11
[3]   NUMERICAL MODELING OF SALT-WATER-INTRUSION AT HALLANDALE, FLORIDA [J].
ANDERSEN, PF ;
MERCER, JW ;
WHITE, HO .
GROUND WATER, 1988, 26 (05) :619-630
[4]  
[Anonymous], 2010, Handbook of Mathematical Functions
[5]  
[Anonymous], 1999, DEV WATER SCI
[6]   The size of the freshwater zone below an elongated island with infiltration [J].
Bakker, M .
WATER RESOURCES RESEARCH, 2000, 36 (01) :109-117
[7]  
Bear J., 1972, DYNAMICS FLUIDS PORO, P764, DOI DOI 10.1097/00010694-197508000-00022.
[8]  
Bolt G.H., 1982, Soil Chemistry, P285
[9]   Response of the salt-freshwater interface in a coastal aquifer to a wave-induced groundwater pulse: field observations and modelling [J].
Cartwright, N ;
Li, L ;
Nielsen, P .
ADVANCES IN WATER RESOURCES, 2004, 27 (03) :297-303
[10]  
Cirkel D. G., 2012, MIXING BEHAV O UNPUB