Cyanamid, Manufacture, Chemistry And Uses
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83.8 55.5 43.2 46.0 Soil calcined 83.8 — — 77.6 Each of the above treatments has diminished the ability of the soil to convert cyanamide to other forms. The calcined soil has very little power of decomposition. It is evident, therefore, that it is not the gross, solid, mineral particles of the soil that have this power, but certain constituents of the soil mass that are destroyed by heat. These constituents belong to the class of chemical compounds that form colloids or disperse systems in the ...soil.
We will now examine the results of experiments made with various materials that are known to form part of practically all soils.
EFFECT OF ZEOUTES.
According to Van Bemmelen^ the colloids of agricultural soil consist principally of amorphous zeolites (amorphous hydrated silicates). These remain for an indeterminate time in suspension in pure water, are coagulated by electrolytes, can be dried into hard compact masses, have in the highest degree the properties of hydrogels, and to their presence is probably due the greater part of the absorptive powers of the soil.
What to read after Cyanamid, Manufacture, Chemistry And Uses?
You can find similar books in the "Read Also" column, or choose other free books by Edward John Pranke to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
83.8 55.5 43.2 46.0 Soil calcined 83.8 — — 77.6 Each of the above treatments has diminished the ability of the soil to convert cyanamide to other forms. The calcined soil has very little power of decomposition. It is evident, therefore, that it is not the gross, solid, mineral particles of the soil that have this power, but certain constituents of the soil mass that are destroyed by heat. These constituents belong to the class of chemical compounds that form colloids or disperse systems in the ...soil.
We will now examine the results of experiments made with various materials that are known to form part of practically all soils.
EFFECT OF ZEOUTES.
According to Van Bemmelen^ the colloids of agricultural soil consist principally of amorphous zeolites (amorphous hydrated silicates). These remain for an indeterminate time in suspension in pure water, are coagulated by electrolytes, can be dried into hard compact masses, have in the highest degree the properties of hydrogels, and to their presence is probably due the greater part of the absorptive powers of the soil.
What to read after Cyanamid, Manufacture, Chemistry And Uses?
You can find similar books in the "Read Also" column, or choose other free books by Edward John Pranke to read onlineMoreLess
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