| LNP Ref#: 4582 | Date: 01-10-11 |
| Origin: ITALY | Lot#: 20101001 |
| Extraction Method: QUARRY |
| Quality: 100% PURE & NATURAL |
| Shelf Life: > THAN 2 YEARS |
| ==================================================================== CHEMICAL ANALYSIS.............PERCENTAGES ==================================================================== SiO2..........................58< X <62 AL2O3.........................15< X <18 Fe2O3.........................3< X <4 MgO...........................5< X <6 K2O...........................0.5< X <1 Na2O..........................0.1< X <0.3 TiO2..........................0.1< X <0.3 CaO...........................3< X <4 MnO...........................Traces P2O5..........................Traces =================================================================== BACTERIOLOGICAL ANALYSIS AVERAGE..............QUANTITY PER G =================================================================== Mesophiles....................................<5000 Pathogenes....................................- Yeast.........................................<50 =================================================================== HEAVY METALS..................................ppm =================================================================== Arsenic.......................................<1 Plomb.........................................<8 Selenium......................................<1 Mercure.......................................<1 Type of Clay: Natural Silicate of aluminium and both, Iron and Magnesium. Major Constituent: Smectite (Montmorillonite) >97% Presentation (dry): Green Clay Powder Cation exchange Capacity (C.E.C): >120 Meq per 100g Adsorbant Power (strychnine Sulfate): >423 mg/g Grit (Another of Montmorillonite): <2.90% Lost of Ignition (1000 deg C): 10.60% Presentation: ==================================================================== This clay come to powder <77um It has to be noted that speaking of a raw mineral chemical analysis is not exactly the same on each part of the quarry without any change of the clay itself. Clay are mainly characterised by X-ray diffraction and cation exchange capacity. By this fact we only give and average value for each component. |
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