Geochemical data on Saratoga mineral waters, applied in deducing a new theory of their origin

Strock, Lester W.

doi:10.2475/ajs.239.12.857

Cited by 16 publications

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“…Radio-chemical quality 5/ 1/51 9/24/52 9/24/52 9/24/52 5/ 1/51 Temperature 2/ 3/55-9/ 4/58 8/30/56-9/ 4/58 prepared by Kemp (1912), Gushing and Kuedemann (1914), Colony (1930), and Strock (1941). Keports by Miller (191 la, 1911b), Gushing and Kuedemann (1914), and Kuedemann (1930), describe the general geology of the area drained by Kayaderosseras and Fish Creeks.…”

Section: Collection and Study Of Rock Cuttings From Test Wells And Comentioning

confidence: 99%

Geology and hydrology of the West Milton area, Saratoga County, New York

Mack¹,

Pauszek²,

Crippen³

1964

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A formation, group of formations, or part of a formation that is waterbearing. Artesian conditions, Occurrence of ground water under sufficient pressure to rise above the level at which it is encountered by a well, but which does not necessarily rise to or above the surface of the ground.-Base flow, Sustained or fair-weather flow. In most streams, base flow is composed largely of groundwater discharge. Bed material, Sediment deposited on the surface of a stream bed. Carbonate hardness, Hardness of water due to calcium and magnesium bicarbonate and (or) carbonate. Clay, Sediment composed of particles having diameters less than 0.004 mm. Color (of water), A visual effect due to material in solution. Cone of depression, The depression, roughly conical in shape, produced in a water table or piezometric surface by pumping (or artesian flow). Correlation, coefficient of, A measure of the degree of relationship between variables. Numerically, the coefficient of correlation (r) ranges from 0 (no correlation) to ± 1 (perfect correlation). The sign is positive if the dependent variable (ordinate value) increases with increases of the independent variable (abscissa value); negative if the dependent variable decreases with an increase in the independent variable. Discharge area, Area of land or body of surface water where ground water discharges naturally directly from the zone of saturation. Dissolved solids, Residue from a clear measured sample of water after evaporation and drying for 1 hour at 180°C. Expressed as parts per million. Drainage area, The area above a specified location that contributes water to a stream. It is measured in a horizontal plane, which is enclosed by a topographic divide in such a way that direct surface runoff from precipitation normally would drain by gravity into the stream above the specified point. Flow-duration curve, A cumulative frequency curve that shows the percentage of time that specified discharges are equaled or exceeded. Fluvial sediment, Fragmental material transported by, suspended in, or deposited by water. Gaging station, A particular site on a stream, canal, lake, or reservoir where systematic observations of gage height or discharge are obtained. A primary gaging station provides a long-term sample of the rate and amount of flow in the hydrologic province for which it serves as an index station. A secondary station provides a short-term sample of rate and flow in an area, which, through correlation techniques, can be related to flow at a primary gaging station. A partial-record station is a particular site where limited streamflow data are collected over a period of years. Ground water, The part of subsurface water that is in the zone of saturation. Hardness, The effect of calcium, magnesium, and other cations having soapconsuming and encrusting properties. Expressed as the calcium carbonate (CaCOs) equivalent in parts per million. m IV GLOSSARY OF TECHNICAL TERMS Mean annual flood, The flood having a recurrence interval of 2.33 years. Micromicro, Prefix meaning 10~12 ; symbo...

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Section: Collection and Study Of Rock Cuttings From Test Wells And Comentioning

confidence: 99%

Geology and hydrology of the West Milton area, Saratoga County, New York

Mack¹,

Pauszek²,

Crippen³

1964

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“…It should have a high degree of plasticity without adhesive properties (no stickiness). 5. It should offer an innate ease of processing.…”

Section: Indicationsmentioning

confidence: 99%

“…Space does not permit a more detailed review of this excellent work, but the reader is referred to it for a most complete review of the subject. 5. Newer Information Regarding Minerals Found in Small Quantities.-With the advent of the spectroscope and the development of new organic compounds for the concentration of various minerals, new tools have become available which are revealing a remarkable picture of elements in the mineral waters which up to the past ten to fifteen years were considered of no importance in the body.…”

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confidence: 99%

Nature of Natural Therapeutic Agents Used at Health Resorts

McClellan¹,

Singer²

1944

JAMA

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“…The mineral zircon is chemically one of the most inert substances known at ordinary temperatures, being virtually unattacked by any known agent, though a trace of solubility in waters containing bicarbonates has been reported (4). Even at elevated temperatures zircon is virtually unattacked by acidic agents; it is, however, decomposed by molten alkalies, forming zirconates which are soluble in aqueous solutions of acids.…”

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Some features of zirconium chemistry.

Blumenthal¹

1949

J. Chem. Educ.

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Tm element zirconium was discovered in 1789 by percentage of dissociation is obtained. If the disso-M. H. Klaproth in the mineral zircon, and was first ciated material is cooled slowly, recombmation of the isolated by J. 3. Berzelius. It occurs widely as a con-two oxides occurs, while if it is quenched, a mixture of stituent of the earth's crust, of which it is estimated the separate oxides is obtained. If the zircon is held to constitute 0.017%. Hence, its abundance is about' at temperatures approximating 2200°C., silica (b. p. equal to that of carbon. The most common ore is 2230"') is volatilized, and a residue consisting largely the orthosilicate, ZrSiO&, but the oxide, baddeleyite, of zirconium dioxide remains. If the zircon is heated also occurs in considerable quantities in Brazil.above the initial decomposition temperature in the About 1% hafnium oxide is generally associated with presence of carbon, the decomposition is promoted and zirconium oxide in its natural occurrences. These two an interesting product called zirconium carbide is elements occupy adjacent spaces in Group IV A of the obtained. Its composition is in agreement with the Periodic Table of Elements, and are virtually identical formula ZrC. The name and stoichiometry of this in chemical properties. It is not possible to separate product are, however, somewhat misleading, suggesting these elements by simple chemical means, and recourse as they do a molecule of the type Zr C. Detailed must be had to tedious recrystallizations or comparable studies of this and similar compounds of other metals techniques. Hence, when speaking of zirconium we point to an "interstitial compound," rather than a generally mean zirconium containing a characteristic molecular compound. In such a compound, the carbon fraction of hafnium.is held in solid solution in the interstices of a metallic According to Sidgwick (2) the electronic structure zirconium crystal skeleton, and the 1:l stoichiometric about the zirconium nucleus can be represented ratio is rather fortuitous. Related compositions are

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Geochemical data on Saratoga mineral waters, applied in deducing a new theory of their origin

Cited by 16 publications

References 0 publications

Geology and hydrology of the West Milton area, Saratoga County, New York

Geology and hydrology of the West Milton area, Saratoga County, New York

Nature of Natural Therapeutic Agents Used at Health Resorts

Some features of zirconium chemistry.

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