Implications of the distribution of δD in pore waters for groundwater flow and the timing of geologic events in a thick aquitard system

被引:119
作者
Hendry, MJ [1 ]
Wassenaar, LI
机构
[1] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada
[2] Environm Canada, Natl Water Res Inst, Saskatoon, SK S7N 3H5, Canada
关键词
D O I
10.1029/1999WR900046
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A detailed vertical profile of the stable isotope delta D in pore water was measured through a thick aquitard system consisting of surficial Quaternary clay-rich till (80 m thick) and an underlying Cretaceous marine clay (76 m thick). Numerical modeling was used to simulate one-dimensional (vertical) groundwater flow and transport of delta D. Best fit simulations to the data provided an independent estimate of long-term groundwater velocity through the aquitard and estimates of the timing of late Pleistocene and Holocene events. Best fit simulations to the measured Isotope profile across the till-clay interface yielded a groundwater velocity of 0.75-1.0 m per 10 ka for a: transport time of between 20 ka and 30 ka. The estimate of velocity agreed well with that calculated from hydraulic data and suggested that hydraulic conductivities of these aquitards are independent of volume tested. The 20-30 ka time frame required for the delta D profile to develop across the till-clay interface reflects the timing of till deposition and shows that the till is the Battleford Formation, a younger till than previously believed. Numerical transport modeling of delta D in the upper 30 m of the profile yielded a nonunique fit. Assuming a similar groundwater velocity to that determined across the till-clay interface, a best fit was obtained for a transport times of 7.5-10 ka. This range compared favorably with that reported for the start of the Holocene (about 10 ka B.P.). This study shows that the application of delta D; and by analogy delta(18)O, to the study of thick aquitard systems not only can provide independent, long-term estimates of very low groundwater velocities but can also provide insight into the timing of major geologic events such as glaciations.
引用
收藏
页码:1751 / 1760
页数:10
相关论文
共 36 条
[21]   Use of vertical profiles of delta O-18 to constrain estimates of hydraulic conductivity in a thick, unfractured aquitard [J].
Remenda, VH ;
vanderKamp, G ;
Cherry, JA .
WATER RESOURCES RESEARCH, 1996, 32 (10) :2979-2987
[22]   ISOTOPIC COMPOSITION OF OLD GROUND-WATER FROM LAKE AGASSIZ - IMPLICATIONS FOR LATE PLEISTOCENE CLIMATE [J].
REMENDA, VH ;
CHERRY, JA ;
EDWARDS, TWD .
SCIENCE, 1994, 266 (5193) :1975-1978
[23]  
ROWE RK, 1997, POLLUTE USERS GUIDE
[24]   GROUNDWATER-FLOW AND SOLUTE TRANSPORT IN FRACTURED LACUSTRINE CLAY NEAR MEXICO-CITY [J].
RUDOLPH, DL ;
CHERRY, JA ;
FARVOLDEN, RN .
WATER RESOURCES RESEARCH, 1991, 27 (09) :2187-2201
[26]   PRECONSOLIDATION PRESSURES IN THE BATTLEFORD FORMATION, SOUTHERN SASKATCHEWAN, CANADA [J].
SAUER, EK ;
CHRISTIANSEN, EA .
CANADIAN JOURNAL OF EARTH SCIENCES, 1991, 28 (10) :1613-1623
[27]   PRECONSOLIDATION OF TILLS AND INTERTILL CLAYS BY GLACIAL LOADING IN SOUTHERN SASKATCHEWAN, CANADA [J].
SAUER, EK ;
EGELAND, AK ;
CHRISTIANSEN, EA .
CANADIAN JOURNAL OF EARTH SCIENCES, 1993, 30 (03) :420-+
[28]  
SHAW J, 1998, IN PRESS CAN GEOTECH
[29]  
SHAW JR, 1998, THESIS U SASK SASKAT
[30]   GROUNDWATER-FLOW, VELOCITY, AND AGE IN A THICK, FINE-GRAINED TILL UNIT IN SOUTHEASTERN WISCONSIN [J].
SIMPKINS, WW ;
BRADBURY, KR .
JOURNAL OF HYDROLOGY, 1992, 132 (1-4) :283-319