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Barbara M. Anderson

Publications and source records attributed to Barbara M. Anderson.

4 recordsLinked to original sources

Trace-metal variation in soils and sagebrush in the Powder River Basin, Wyoming and Montana

A reconnaissance study of 28 trace metals in samples of surface soil (0-2.5 cm deep), subsurface soil (15-20 cm deep), and big sagebrush ( Artemisia tridentata ) that were collected from the Powder River Basin in Wyoming and Montana indicates that little variation occurs in nature at scales greater than about 35 km. This general lack of broadscale variation suggests that simple summary statistics for these materials could provide basinwide geochemical baselines for use in monitoring secular changes in the local geochemical environment. Samples of big sagebrush near the Dave Johnston Power Plant at the southern edge of the basin exhibit statistically significant reductions of strontium, vanadium, uranium, and selenium eastward from the plant.

Montana, Wyoming

Lithium in surface and ground waters of the conterminous United States

The accompanying map, which shows concentrations of lithium in surface and ground caters of the conterminous United States, was compiled at the request of Helen Cannon (U.S. Geological Survey) for use at the Workshop on Geochemical Environment in Relation to Health and Disease. The workshop was held February 6-12, 1972, in Pacific Grove, California. The lithium study group, led by Dr. Walter Mertz (U.S. Department of Agriculture), met to discuss the possible protective action of lithium (Livingston, 1970; Steinberg, 1970; Voors, 1969, 1970) against atherosclerotic heart disease. The map will be published in the findings of the workshop by the National Academy of Sciences, opposite a h; art disease map compiled by Herbert 1. Sauer (University of Missouri).

Open-File Report

Calcium-Carbonate hardness of public water supplies in the conterminous United States

Geographic variations in the hardness of water seem to parallel the geographic variations in certain cardiovascular diseases (Anderson and others, 1969; Biorck and others, 1965; Schroeder, 1966). Winton and McCabe (1970) have provided a recent review of the problem. The map, presented here, showing calcium-carbonate hardness of municipal raw-water sources in the conterminous United States has been compiled to provide data for further examination of correlations between water hardness and cardiovascular diseases.

Book chapter

The geochemist’s involvement with the pollution problem

The geochemist can contribute much information of value toward assessing the effect of environment, including inorganic pollution, on health. The average composition of rocks, soils, plants, and water and also the increments of inorganic substances that can be expected in geologic environments of high-metal content are essential for comparison with metal contents of these components of the environment in areas contaminated by various types of inorganic air and water pollution. Background levels of lead, zinc, nickel, chromium, copper, and manganese in soils and in four classes of vegetation have been estimated from collections that were made in remote areas presumed to be free from inorganic contamination. The trace-metal content of soils and plants varies widely in different geologic provinces of the United States; in those areas of high natural mineralization, additions of metals from man-made pollution may compound a possible hazard. Results of sampling in urban areas show that contamination of vegetation by gasoline lead can be expected for at least 1000 ft back from transportation lanes, and that the lead burden is increasing greatly with time. Ore-treatment plants can also be a source of air contamination for several miles downwind and several thousand feet in other directions. Soils of naturally high metal content in a mining district may be further contaminated with both major and minor elements from smelting operations. Recent studies show that volatile elements are released directly to the air from ore deposits in place. Concentrations of mercury, for instance, may be as much as 20 times background for several hundred feet in altitude over ore deposits in which mercury occurs as a relatively minor constituent. The source of inorganic pollution in surface drainage and also in ground water is commonly geologic, as rivers may be contaminated from coal and metal deposits in place and also from mining and smelting operations. More information of the type illustrated should be accumulated and made available to scientists who are working in environmental health, and, in particular, to those involved in the pollution problem. Only by these means can we provide a scientific basis for the enactment of realistic and effective legislation for pollution control.

Book chapter