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Precipitation rates (R) were calculated from the amount of calcite precipitated, growth time, and specific surface area.
Thermodynamics only indicates if considered minerals can precipitate or not but does not provide any information about the precipitation rates.
The National Space Development Agency of Japan contributed a microwave scanning radiometer to measure water vapor content and precipitation rates, and Brazil's space agency provided a device to measure atmospheric humidity.
The daily precipitation rates were also plotted.
Fast demixing process (higher precipitation rates) forms finer pores while delayed demixing process (slow precipitation rates) results in rough structures.
Both figures include five maps showing the daily precipitation rates for days 3 7.
With lower precipitation rates, all vegetation types showed comparable evapotranspiration rates due to water limitations.
However, precipitation rates at fixed saturation states also evolved with time.
Average precipitation rates of the four sites differ from 110 to 250 mm/year.
Precipitation rates accelerated for low r values but slowed for high r values.
In both figures, areas with high precipitation rates are highlighted in dark blue.
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