Structure and Mineralogical Properties
Classic Neuburg Siliceous Earth is a natural combination of corpuscular, crypto-crystalline and amorphous silica and lamellar kaolinite: a loose mixture impossible to separate by physical methods. As a result of natural aging, the silica portion exhibits a round grain shape and consists of aggregated, crypto-crystalline primary particles of about 200 nm diameter which are coated partially opal-like. Such a unique structure is responsible for a relatively high specific area and oil absorption, which result, besides rheological activity, also in a whole range of application advantages.
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Silica (corpuscular), |
Kaolinite (lamellar), |
Neuburg Siliceous Earth |



