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- W2060565463 abstract "The characterization of colloids from the Grimsel Test Site granitic groundwater has been carried out after concentrating the natural colloids by diaultrafiltration in situ and in the laboratory. A 2-year-long study has shown little variation in the chemistry of the Grimsel water (T = 285K, pH = 9.6) and a calculation of saturation indices indicates that quartz and fluorite are slightly oversaturated in the in situ conditions (log P(CO2)/atm. = −5.5). Scanning electron microscope (SEM) investigations indicate a colloid concentration of approximately 1010 particles (40 to 1000 nm) per litre. On the basis electron spectroscopy for chemical analysis (ESCA), transmission electron microscopy (TEM), energy dispersive X-ray spectrometry (EDS), electron energy loss spectrometry (EELS), and laser microprobe mass analysis (LAMMA), the particles are a mixture of organic (C, N, O, (S)) and inorganic (Si, Ca, S and to a lesser extent Mg, Sr and Ba) materials. The alpha specific activity in the colloidal phase is less than 0.5 mBq · 1−1. The mode of formation is discussed together with the size distribution and the concentration." @default.
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- W2060565463 date "1989-03-01" @default.
- W2060565463 modified "2023-10-03" @default.
- W2060565463 title "Colloids in water from a subsurface fracture in granitic rock, Grimsel Test Site, Switzerland" @default.
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- W2060565463 doi "https://doi.org/10.1016/0016-7037(89)90003-3" @default.
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