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CO: WRIND3 <br /> YR: 1991 <br /> PD: sketch map <br /> CN: U. S. Geological Survey Toxic Substances Hydrology Program, <br /> technical meeting, Monterey, CA, March 11-15, 1991 <br /> LA: English <br /> DE: Massachusetts-; hydrogeology-; ground-water; aquifers-; <br /> heterogeneity-; USGS-; New-England; Eastern-U.S. ; United-States; <br /> southeastern-Massachusetts; Barnstable-County-Massachusetts; <br /> Cape-Cod; Eastern-United-States; pollution-; sewage-; <br /> polluted-water; waste-disposal; tracers-; <br /> physicochemical-properties; microorganisms-; transport-; <br /> bromide-ion <br /> DT: Analytic; Serial; Report; Conference publication <br /> MC: 1AT: N413600; N413900; LONG: W0703200; W0703500 <br /> CC: 21-Hydrogeology-and-hydrology; 02-Geochemistry; <br /> 22-Environmental-geology <br /> SB: B; Bibliography and Index of Geology (1969-present) <br /> IS: 0092-332X <br /> RN: WRI 91-4034 <br /> AV: U. S. Geol. Surv. , Denver, CO, United States <br /> GEOREF Disc 3 <br /> 22 of 60 <br /> AN: 94-17380 <br /> TI: Field-scale solute transport; spatially interpolating the <br /> parameters of a transfer function model. <br /> AU: Hosang-Juerg <br /> OS: University of Basel, Department of Geography, Geoecology <br /> Research Group, Basel, Switzerland; Agricultural University, <br /> Wageningen, Netherlands <br /> SO: Wagenet, R. J. , Bouma, J. Special issue; Operational methods <br /> to characterize soil behavior in space and time. Cornell <br /> University, Department of Soil, Crop and Atmospheric Sciences, <br /> Ithaca, NY, United-States. Geoderma. 60. (1-4) . p. 119-133 . <br /> 13 Refs. <br /> CO: GEDMAB <br /> YR: 1993 <br /> PD: illus. , 3 tables, sketch maps <br /> CN: 1992 conference of Working Group M/V of the International <br /> Society of Soil Science, Ithaca, NY, July 26-29, 1992 <br /> LA: English <br /> AB: The results from a solute transport study done near Basel, <br /> Switzerland are reported. The experimental site was a 3 .25 ha <br /> corn field consisting of well drained silt loam. A bromide tracer <br /> was applied to the surface of 40 plots, located at regular <br /> intervals on a grid. Soil cores were taken twice at each plot <br /> during the experiment. The first time, samples were collected at <br /> 10 cm intervals from the surface to 50 cm. During the second <br /> sampling, soil cores were taken to a depth of 100 cm in 20 cm <br /> increments. Four plots were sampled twice each time to assess <br /> small-scale heterogeneities. Solute transport was described as a <br /> convective-dispersive process with highly variable parameters <br /> within the test field. A poor correspondence between the apparent <br />