COMPOSITIONS CONTAINING A SOURCE OF HYPOCHLORITE IONS

• US 3,843,548 A
• Filed: 09/28/1971
• Issued: 10/22/1974
• Est. Priority Date: 10/06/1970
• Status: Expired due to Term

• Current Assignee: , James R.
• Original Assignee: , James R.
• Inventors: JAMES R
• Application Number:
  US05/184,510
• Time in Patent Office: 1,120 Days
• US Class Current: 252/187.26
• CPC Class Codes: A61K 47/02 Inorganic compounds
• CPC Class Codes: A61K 9/12 Aerosols; Foams A61K9/0043, A61K9/0056, A61K9/006, A61K9/0073 take precedence; spray-films A61K9/7015
• CPC Class Codes: B01J 20/10 comprising silica or silicate
• CPC Class Codes: B65D 35/22 with two or more compartments
• CPC Class Codes: C01B 33/20 Silicates persilicates C01B15/14 ; containing aluminium C01B33/26
• CPC Class Codes: C11D 3/3956 Liquid compositions

Abstract

1. A COMPOSITION CONSISTING ESSENTIALLY OF A WATERABSORPTIVE CLAY AND A SOURCE OF HYPOCHLORITE IONS, SAID SOURCE OF HYPOCHLORITE IONS BEING A MEMBER SELECTED FROM THE GROUP CONSISTING OF ALKALI METAL HYPOCHLORITES, ALKALI METAL SALTS OF NON-METALLIC INORGANIC ACIDS, AND ORGANIC ACIDS CONTAINING A THERMODYNAMICALLY STABLE NITROGEN-CHLORINE BOND WHICH HYDROLYSES TO PROVIDE HYPOCHLORITE IONS, WHEREIN SAID WATER-ABSORPTIVE CLAY IS A SYNTHETIC MAGNESIUM SILICATE IN WHICH A PROPORTION OF THE MAGNESIUM ATOMS HAVE BEEN REPLACED BY LITHIUM ATOMS, SAID SYNTHETIC MAGNESIUM SILICATE BEING PRESENT IN AN AMOUNT OF FROM ABOUT 3% TO 8% BY WEIGHT, THE AMOUNT OF SAID SOURCE OF HYPOCHLORITE IONS BEING SUCH THAT THE AVAILABLE CHLORINE CONTENT OF SAID COMPOSITION IS FROM 0.05% TO 3.0% BY WEIGHT.

Claims

1. A COMPOSITION CONSISTING ESSENTIALLY OF A WATERABSORPTIVE CLAY AND A SOURCE OF HYPOCHLORITE IONS, SAID SOURCE OF HYPOCHLORITE IONS BEING A MEMBER SELECTED FROM THE GROUP CONSISTING OF ALKALI METAL HYPOCHLORITES, ALKALI METAL SALTS OF NON-METALLIC INORGANIC ACIDS, AND ORGANIC ACIDS CONTAINING A THERMODYNAMICALLY STABLE NITROGEN-CHLORINE BOND WHICH HYDROLYSES TO PROVIDE HYPOCHLORITE IONS, WHEREIN SAID WATER-ABSORPTIVE CLAY IS A SYNTHETIC MAGNESIUM SILICATE IN WHICH A PROPORTION OF THE MAGNESIUM ATOMS HAVE BEEN REPLACED BY LITHIUM ATOMS, SAID SYNTHETIC MAGNESIUM SILICATE BEING PRESENT IN AN AMOUNT OF FROM ABOUT 3% TO 8% BY WEIGHT, THE AMOUNT OF SAID SOURCE OF HYPOCHLORITE IONS BEING SUCH THAT THE AVAILABLE CHLORINE CONTENT OF SAID COMPOSITION IS FROM 0.05% TO 3.0% BY WEIGHT.