Disertacion sobre el origen de la termalidad de las aguas minero-medicinales /

Mode of access: Internet.

Desenvolvimento de sensores químicos para aniões

O objectivo deste trabalho foi o desenvolvimento de sensores químicos para aniões em solução aquosa. Os sensores basearam-se em cristais piezoelétricos de quartzo revestidos com macrociclos pirrólicos. Sensores com porfirinas, hexafirinas, ftalocianinas e uma rede metalo-orgânica como filmes de reconhecimento foram avaliados no que respeita à reversibilidade, sensibilidade, seletividade e tempo de vida. A sensibilidade aos aniões presentes nas águas minerais destinadas ao consumo humano dos sensores com macrociclos pirrólicos dependia dos grupos substituintes na periferia do macrociclo. A presença de grupos substituintes NH potenciou a sensibilidade, sendo o valor mais elevado obtido com o grupo NH-tosilo. Técnicas espectroscópicas permitiram mostrar que a principal interação entre o anião e o composto se fazia por meio de pontes de hidrogénio entre o anião e o grupo NH. A sensibilidade destes compostos dependia ainda da quantidade do composto depositado sobre o cristal. Nenhum dos sensores era específico, mas apresentavam variações na seletividade com o composto pirrólico sobre o cristal. O sensor com uma membrana polimérica que incorporou uma rede metalo-orgânica construída com moléculas de uma ftalocianina de magnésio com grupos NH-tosilo ligados por iões cobre apresentou coeficientes de seletividade muito diferentes de todos os restantes sensores. Uma língua eletrónica construída com três dos novos sensores foi capaz de determinar simultaneamente as concentrações dos iões HCO3-, Cl- e SO42- em amostras de água mineral engarrafada, não tendo os valores obtidos sido estatisticamente diferentes (α=0,05) daqueles que foram obtidos por cromatografia iónica ou volumetria.

The ionic composition of surface waters in the English Lake District, related to bedrock geology, with some singular facts and speculation on the existence of mineral-rich groundwaters

This article is based on a survey of tarns conducted mainly in the summers of 1983 to 1985, plus a survey made in the winter of 1985, in which streams were sampled on the wide variety of rock-types occurring on the fringes of the Lake District. Differences in composition of major ions and their concentrations in the surface waters of Cumbria reflect the complex geological structure of the region. At altitudes above 300 m, on Borrowdale Volcanics and Skiddaw Slates, surface waters are derived from atmospheric precipitation, with additional inputs of some ions - especially calcium and bicarbonate - from catchment rocks and soils. In some of the low-lying large lakes on the fringes of the central fells, water composition is also dominated by inputs from upper catchments; examples are Wastwater, Ullswater and Haweswater. However in other lakes there is evidence (Derwentwater and Bassenthwaite Lake) of inputs from saline groundwater.

(Table 2) Concentrations of particulate chemical elements in waters of the Pechora Sea

Mineralogy of suspended matter from surface and bottom waters has been studied at two sites in the Barents Sea. Along with terrigenous minerals, particulate matter samples contain authigenic mineral phases of iron and manganese oxyhydroxides. Mn-feroxyhite, Fe-vernadite, goethite, and proto-ferrihydrite have been identified in samples from the surface waters, whereas birnessite and non-ferruginous vernadite have been found in samples from the bottom waters. Formation of suspended manganese minerals in the bottom waters is explained by an additional Mn supply from underlying reduced sediments during their early diagenesis and oxygen depletion in the near-bottom nepheloid layer. Bacteria are supposed to take part in the authigenic mineral formation.

(Table 2) Vertical distribution of particulate matter and its organic and mineral components in waters of the Tropical Atlantic in November 1984

Results of multiyear investigation of distribution and composition of suspended matter in waters off the northwest coast of Africa are presented. Large-scale circulation, upwelling, river runoff, and aeolian deposition affect distribution and evolution of biochemical composition of particulate matter. Concentrations of organic carbon, nitrogen, chlorophyll, phytoplankton and trace metals in the particulate matter are determined. Ratios of these components exhibit seasonal variations.

Sulphate and d34S in pore waters and d13C, d18O and mineral composition of carbonate nodules from ODP Leg 188 sites

Carbon and oxygen isotopic compositions of authigenic carbonate nodules or layers reflect the diagenetic conditions at the time of nodule growth. The shallowest samples of carbonate nodules and dissolved inorganic carbon of pore water samples beneath the sulfate reduction zone (0-160 meters below seafloor [mbsf]) at Site 1165 have extremely negative d13C values (-50 per mil and -62 per mil, respectively). These negative d13C values indicate nodule formation in association with anaerobic methane oxidation coupled with sulfate reduction. The 34S of residual sulfate at Site 1165 shows only minor 34S enrichment (+6 per mil), even with complete sulfate reduction. This small degree of apparent 34S enrichment is due to extreme "open-system" sulfate reduction, with sulfate abundantly resupplied by diffusion from overlying seawater. Ten calcite nodules from Site 1165 contain minor quartz and feldspar and have d13C values ranging from -49.7 per mil to -8.2 per mil. The nodules with the most negative d13C values currently are at depths of 273 to 350 mbsf and must have precipitated from carbonate largely derived from subsurface anaerobic methane oxidation. The processes of sulfate reduction coupled with methane oxidation in sediments of Hole 1165B are indicated by characteristic concentration and isotopic (d34S and d13C) profiles of dissolved sulfate and bicarbonate. Three siderite nodules from Site 1166 contain feldspar and mica and one has significant carbonate-apatite. The siderite has d13C values ranging from -15.3 per mil to -7.6 per mil. These siderite nodules probably represent early diagenetic carbonate precipitation during microbial methanogenesis.

A short history of Brighthelmston, with remarks on its air, and an analysis of its waters, particularly of an uncommon mineral one long discovered, though but lately used.

Published in 1761; re-edited 1829 by James Charles Michell.

The Virginia tourist. Sketches of the springs and mountains of Virginia: containing an eexposition of fields for the touist la Virginia; natural beauties and wonders of the state; also accounts of its mineral springs: and a medical guide to the use of the waters. etc., etc.

Mode of access: Internet.

(Table 1) Mineral phosphorus contents in bottom sediments and interstitial waters of the Southeast Atlantic

Concentrations of mineral phosphorus in interstitial waters from sediments of the Southeast Atlantic generally increases from the ocean bed to the continental slope and shelf. In diatomaceous oozes of the Southwest Africa shelf, phosphorus concentration in fresh interstitial waters reaches 2.5 mg/l in absence of phosphorite concretions and 0.1-0.7 mg/l in their presence. After prolonged storage of samples concentration of dissolved mineral phosphorus sometimes increases up to 7-8 mg/l. The key factor regulating phosphorus content of solid and liquid phases of unaltered sediments are content and composition of organic matter.