DETERMINATION OF SUBSURFACE FLUID CONTENTS AT A CRUDE-OIL SPILL SITE

被引:22
作者
HESS, KM [1 ]
HERKELRATH, WN [1 ]
ESSAID, HI [1 ]
机构
[1] US GEOL SURVEY,MENLO PK,CA 94025
关键词
D O I
10.1016/0169-7722(92)90044-F
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Measurement of the fluid-content distribution at sites contaminated by immiscible fluids, including crude oil, is needed to better understand the movement of these fluids in the subsurface and to provide data to calibrate and verify numerical models and geophysical methods. A laboratory method was used to quantify the fluid contents of 146 core sections retrieved from boreholes aligned along a 120-m longitudinal transect at a crude-oil spill site near Bemidji, Minnesota, U.S.A. The 47-mm-diameter, minimally disturbed cores spanned a 4-m vertical interval contaminated by oil. Cores were frozen on site in a dry ice-alcohol bath to prevent redistribution and loss of fluids while sectioning the cores. We gravimetrically determined oil and water contents using a two-step method: (1) samples were slurried and the oil was removed by absorption onto strips of hydrophobic porous polyethylene (PPE); and (2) the samples were oven-dried to remove the water. The resulting data show sharp vertical gradients in the water and oil contents and a clearly defined oil body. The subsurface distribution is complex and appears to be influenced by sediment heterogeneities and water-table fluctuations. The center of the oil body has depressed the water-saturated zone boundary, and the oil is migrating laterally within the capillary fringe. The oil contents are as high as 0.3 cm3 cm-3, which indicates that oil is probably still mobile 10 years after the spill occurred. The thickness of oil measured in wells suggests that accumulated thickness in wells is a poor indicator of the actual distribution of oil in the subsurface. Several possible sources of error are identified with the field and laboratory methods. An error analysis indicates that adsorption of water and sediment into the PPE adds as much as 4% to the measured oil masses and that uncertainties in the calculated sample volume and the assumed oil density introduce an additional +/- 3% error when the masses are converted to fluid contents.
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页码:75 / 96
页数:22
相关论文
共 21 条
[1]   LIMITATIONS OF MONITORING WELLS FOR THE DETECTION AND QUANTIFICATION OF PETROLEUM-PRODUCTS IN SOILS AND AQUIFERS [J].
ABDUL, AS ;
KIA, SF ;
GIBSON, TL .
GROUND WATER MONITORING AND REMEDIATION, 1989, 9 (02) :90-99
[2]  
ABDUL AS, 1991, J HYDROL, V121, P133
[3]  
Baedecker M. J., 1984, US GEOL SURV TOX WAS, P65
[4]   SELECTIVE TRANSPORT OF HYDROCARBONS IN THE UNSATURATED ZONE DUE TO AQUEOUS AND VAPOR-PHASE PARTITIONING [J].
BAEHR, AL .
WATER RESOURCES RESEARCH, 1987, 23 (10) :1926-1938
[5]   ASSAY OF ORGANIC LIQUID CONTENTS IN PREDOMINANTLY WATER-WET UNCONSOLIDATED POROUS-MEDIA [J].
CARY, JW ;
MCBRIDE, JF ;
SIMMONS, CS .
JOURNAL OF CONTAMINANT HYDROLOGY, 1991, 8 (02) :135-142
[6]  
CRAWFORD JG, 1958, SUBSURFACE GEOLOGY P, P229
[7]   LNAPL DISTRIBUTION IN A COHESIONLESS SOIL - A FIELD INVESTIGATION AND CRYOGENIC SAMPLER [J].
DURNFORD, D ;
BROOKMAN, J ;
BILLICA, J ;
MILLIGAN, J .
GROUND WATER MONITORING AND REMEDIATION, 1991, 11 (03) :115-122
[8]  
ESSAID HI, 1991, US GEOLOGICAL SURVEY, P614
[9]   VOLUME ESTIMATION OF LIGHT NONAQUEOUS PHASE LIQUIDS IN POROUS-MEDIA [J].
FARR, AM ;
HOUGHTALEN, RJ ;
MCWHORTER, DB .
GROUND WATER, 1990, 28 (01) :48-56
[10]  
Franzi D., 1988, US GEOLOGICAL SURVEY, pC5