‡Saturation index expressed in logarithmic form:
If calcite dissolves much more rapidly than dolomite, calcite saturation would be attained much before dolomite saturation.
(4) Limestone (calcite) Closed-system dissolution of calcite to saturation 3.9 8.4 31 0 35 8.9 10–4.4 1 0
The definition of this water assumes saturation with respect to calcite, baryte, fluorite, chalcedony, and kaolinite.
The definition of this water assumes saturation with respect to calcite, baryte, fluorites, chalcedony, and kaolinite.
During infiltration, saturation with respect to calcite is attained by open-system dissolution.
Thus, the saturation index (SIc) for calcite is large, as indicated in Table 7.7.
If dolomite saturation is attained quickly, there would be little opportunity for calcite to dissolve.
If groundwater at 10°C dissolves dolomite to saturation and then flows into a zone that contains calcite, no calcite dissolution will occur, because the water would be saturated with respect to calcite.
In terms of equilibrium constants and activities, the saturation conditions for calcite and dolomite can be expressed as
Powdered calcite is often used as a white pigment or "whiting.
Calcite powder is often used as a white pigment or "whiting".
Powdered calcite is often used as a white pigment or "whiting".
Large transparent crystals of calcite are called Iceland spar.
Also, the calculation factor can be triggered in this menu, an LSI (Langelier Saturation Index) and RSI (Rysnar Stability Index).
The saturated state of the hit rate is judged as a sign of breakage.
Line (1) represents the initial condition for the CO2 charged water; line (2) represents calcite saturation; line (3) represents dolomite saturation if dolomite is dissolved under similar conditions.
In this case, a* and b* represent a chromaticness index defined in the CIELAB color space.
Using isosbestic points and curve areas, a relative saturation index was calculated.
Honey calcite is also known as amber or gold calcite.
Groundwater at a temperature of 25°C moves through a limestone bed where it attains saturation with respect to calcite.
Inline Alkaline Calcite/Corosec filter : Calcite is a naturally occurring calcium carbonate media.
Water from rain and snow that infiltrates into terrain containing calcite and dolomite normally dissolves these minerals to saturation levels.
Synthetic sketch describing the hypothesis for the formation of the needle fiber calcite and calcitic nanofibers (PhD thesis Bindschedler S., 2011)
A sodium index may be determined and used in conjunction with one or more other logs to determine a saturation of the subsurface formation.
The reference value may be, for example, determined by an oxygen (02) variation index that indicates a change in blood oxygen saturation of tissue.
The oxygen saturation sensor obtains the oxygen saturation level of the user.
When the water moves from the sandstone into the limestone, dissolution of calcite to saturation causes the pH to rise to 8.9 as H+ is consumed by the conversion of dissolved CO2 to .
Today we are going to discuss catching in general.
Requêtes fréquentes français :1-200, -1k, -2k, -3k, -4k, -5k, -7k, -10k, -20k, -40k, -100k, -200k, -500k, -1000k,
Requêtes fréquentes anglais :1-200, -1k, -2k, -3k, -4k, -5k, -7k, -10k, -20k, -40k, -100k, -200k, -500k, -1000k,
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