|
|
||||||||
1 Western Dairy Center, Department of Nutrition and Food Sciences, Utah State University, Logan, UT 84322-8700
2 Department of Microbiology, Weber State University, Ogden UT 84408-2506
Salted and unsalted nonfat mozzarella cheese was made by direct acidification and stored at 4°C over 60 d. Changes in cheese opacity were measured by using reflectance L* values while the cheese was heated from 10 to 90°C, then cooled to 10°C, and reheated to 90°C. A characteristic opacity transition temperature (TOP) was obtained for each cheese. Both salt content and storage time influenced TOP. Opacity during heating, cooling, and reheating formed a hysteresis. At d 1, the unsalted cheese became opaque when heated to 20°C, but the salted cheese required heating to 40°C. As the salted cheese was aged, its TOP increased so that by 60 d the cheese did not become opaque until it was heated to 70°C.
Key Words: cheese opacity salt storage direct acidification
Submitted on December 7, 2000
Accepted on June 6, 2001
This article has been cited by other articles:
![]() |
N. S. Joshi, K. Muthukumarappan, and R. I. Dave Understanding the Role of Calcium in Functionality of Part Skim Mozzarella Cheese J Dairy Sci, June 1, 2003; 86(6): 1918 - 1926. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. J. Pastorino, R. I. Dave, C. J. Oberg, and D. J. McMahon Temperature Effect on Structure-Opacity Relationships of Nonfat Mozzarella Cheese J Dairy Sci, September 1, 2002; 85(9): 2106 - 2113. [Abstract] [Full Text] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |