Prediction of local concentration statistics in variably saturated soils: Influence of observation scale and comparison with field data

被引:15
作者
Graham, W
Destouni, G
Demmy, G
Foussereau, X
机构
[1] Univ Florida, Inter Disciplinary Program Hydrol Sci, Gainesville, FL 32611 USA
[2] Royal Inst Technol, Dept Civil & Environm Engn, S-10044 Stockholm, Sweden
关键词
stochastic modeling; subsurface flow and transport; vadose zone;
D O I
10.1016/S0169-7722(97)00089-2
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The methodology developed in Destouni and Graham [Destouni, G., Graham, W.D., 1997. The influence of observation method on local concentration statistics in the subsurface. Water Resour. Res. 33 (4) 663-676.] for predicting locally measured concentration statistics :For solute transport in heterogeneous porous media under saturated flow conditions is applied to the prediction of conservative nonreactive solute transport in the vadose zone where observations are obtained by soil coring. Exact analytical solutions are developed for both the mean and variance of solute concentrations measured in discrete soil cores using a simplified physical model for vadose-zone flow and solute transport. Theoretical results show that while the ensemble mean concentration is relatively insensitive to the length-scale of the measurement, predictions of the concentration variance are significantly impacted by the sampling interval. Results also show that accounting for vertical heterogeneity in the soil profile results in significantly less spreading in the mean and variance of the measured solute breakthrough curves, indicating that it is important to account for vertical heterogeneity even for relatively small travel distances. Model predictions for both the mean and variance of locally measured solute concentration, based on independently estimated model parameters, agree well with data from a field tracer test conducted in Manatee County, Florida. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:177 / 199
页数:23
相关论文
共 37 条
[1]  
BRESLER E, 1981, WATER RESOUR RES, V17, P683
[2]   FIELD SCALE TRANSPORT OF BROMIDE IN AN UNSATURATED SOIL .1. EXPERIMENTAL METHODOLOGY AND RESULTS [J].
BUTTERS, GL ;
JURY, WA ;
ERNST, FF .
WATER RESOURCES RESEARCH, 1989, 25 (07) :1575-1581
[3]   FIELD SCALE TRANSPORT OF BROMIDE IN AN UNSATURATED SOIL .2. DISPERSION MODELING [J].
BUTTERS, GL ;
JURY, WA .
WATER RESOURCES RESEARCH, 1989, 25 (07) :1583-1589
[4]   A SOLUTE FLUX APPROACH TO TRANSPORT IN HETEROGENEOUS FORMATIONS .2. UNCERTAINTY ANALYSIS [J].
CVETKOVIC, V ;
SHAPIRO, AM ;
DAGAN, G .
WATER RESOURCES RESEARCH, 1992, 28 (05) :1377-1388
[5]   TRANSPORT OF KINETICALLY SORBING SOLUTE BY STEADY RANDOM VELOCITY IN HETEROGENEOUS POROUS FORMATIONS [J].
CVETKOVIC, V ;
DAGAN, G .
JOURNAL OF FLUID MECHANICS, 1994, 265 :189-215
[6]   THEORY OF SOLUTE TRANSPORT BY GROUNDWATER [J].
DAGAN, G .
ANNUAL REVIEW OF FLUID MECHANICS, 1987, 19 :183-215
[7]   A SOLUTE FLUX APPROACH TO TRANSPORT IN HETEROGENEOUS FORMATIONS .1. THE GENERAL FRAMEWORK [J].
DAGAN, G ;
CVETKOVIC, V ;
SHAPIRO, A .
WATER RESOURCES RESEARCH, 1992, 28 (05) :1369-1376
[8]   SOLUTE-DISPERSION IN UNSATURATED HETEROGENEOUS SOIL AT FIELD SCALE .1. THEORY [J].
DAGAN, G ;
BRESLER, E .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1979, 43 (03) :461-467
[9]   Stochastic analysis of concentration measurements in the transport experiment at Twin Lake site [J].
Dagan, G ;
Indelman, P ;
Moltyaner, G .
WATER RESOURCES RESEARCH, 1997, 33 (04) :559-567
[10]   SOLUTE TRANSPORT IN HETEROGENEOUS POROUS FORMATIONS [J].
DAGAN, G .
JOURNAL OF FLUID MECHANICS, 1984, 145 (AUG) :151-177