Neuburg Siliceous Earth
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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.

  • Quick Incorporation
  • No Filler Agglomeration
  • Minimal Sedimentation
  • Excellent Dispersion
  • High Surface Activity
  • Excellent Extrusions Properties
  • Low Compression Set in Rubber Goods
  • Excellent Scratch Resistance in Plastics, Paints and Varnishes
 

 

Silica
plus
Kaolinite
ist
Neuburg Siliceous Earth

Silica (corpuscular),
 Neuburg Siliceous Earth (18.000x)

 

 Kaolinite (lamellar),
 (15.000x)

 

 Neuburg Siliceous Earth
 (loose structure 10.000x)