Exopolysaccharides in sourdough fermented by Weissella confusa QS813 protected protein matrix and quality of frozen gluten-red bean dough during freeze-thaw cycles

2021 ◽  
pp. 101180
Author(s):  
Binle Zhang ◽  
Jacob Ojobi Omedi ◽  
Jianxian Zheng ◽  
Weining Huang ◽  
Chunli Jia ◽  
...  
1977 ◽  
Vol 34 (12) ◽  
pp. 2369-2373 ◽  
Author(s):  
Doris Fraser Hiltz ◽  
D. H. North ◽  
Barbara Smith Lall ◽  
R. A. Keith

Refrozen silver hake (Merluccius bilinearis), processed as fillets and minced flesh after thawing of stored round fish that had been frozen within 14 h of capture, underwent rapid deterioration during storage at −18 °C compared with once-frozen control materials from the same lot of fish. The estimated maximum storage life of silver hake refrozen as fillets after 3 and 6 mo storage of the round fish at −25 °C was reduced to about 4.5 and 1 mo, respectively, from 10 mo for once-frozen control fillets. Quality of the refrozen materials immediately after thawing and refreezing was similar to that of the round-frozen fish, except after 6 mo, where some initial deterioration occurred, particularly in minced flesh. Minced flesh was more unstable in frozen storage than fillets. In all once- and twice-frozen materials, formation of dimethylamine occurred concomitantly with decrease in protein extractability. Round-frozen fish underwent no loss in protein extractability during 6 mo storage at −25 °C, but some lipid hydrolysis occurred. These results suggest that the freeze–thaw–refreeze process as applied to silver hake will yield a final product of acceptable quality provided that storage of the round fish does not exceed 3–4 mo and that the refrozen materials are marketed within a month after processing. Key words: silver hake, Merluccius bilinearis, refrozen storage, dimethylamine, minced flesh


2009 ◽  
Vol 58 (1) ◽  
pp. 70-85
Author(s):  
Henry Munack ◽  
Hilmar Schröder

Abstract. Ground temperature measurements have been carried out at eleven different sites of the Prokhodnaja valley in the high mountains of the Zailijskij Alatau (Northern Tian Shan, Kazakhstan) between the summers of 2003 and 2004. For this purpose the periglacial zone and adjacent altitudinal zones have been examined between 2,500 and 4,000 m asl with an equidistance of 250 m. The influences of the altitude, the exposure as well as the depth below the earth’s surface on the thermal content and condition of periglacial soils have been considered. The measurements provide useful information about the relations between quantity and quality of freeze-thaw action and the parameters mentioned above.


2005 ◽  
Vol 16 (4) ◽  
pp. 354-378 ◽  
Author(s):  
S. JITTINANDANA ◽  
P.B. KENNEY ◽  
S.D. SLIDER
Keyword(s):  

2020 ◽  
Vol 43 (11) ◽  
Author(s):  
Hongyao Jiang ◽  
Min Zhang ◽  
Yanan Sun ◽  
Bhesh Bhandari ◽  
Xi Wang

2020 ◽  
Vol 65 ◽  
pp. 102454 ◽  
Author(s):  
Jiaheng Li ◽  
Jiyong Shi ◽  
Xiaowei Huang ◽  
Xiaobo Zou ◽  
Zhihua Li ◽  
...  

2019 ◽  
Vol 35 (03) ◽  
pp. 262-270
Author(s):  
Yuxia Zhao ◽  
Yujin Moon ◽  
Woosung Bae ◽  
Choongwoo Nam ◽  
Meera Kweon

1944 ◽  
Vol 6c (3) ◽  
pp. 209-216 ◽  
Author(s):  
J. C. Medcof

Low quality shells are easily broken, have a high water content and low specific gravity, and contain little pearly and much chalky material. Pearly shell is secreted throughout the season before and after the chalk which it incloses. Chalky areas occur in all shells, have functional importance, are commonest in oysters that are poorest in late summer and are regular in their order of appearance and position on the shell. They are composed of large vertical calcite crystals in a porous mass of smaller crystals with a protein matrix.


1991 ◽  
Vol 18 (4) ◽  
pp. 681-689 ◽  
Author(s):  
C. James Martel ◽  
Carl J. Diener

In 1986, a pilot-scale sludge freezing bed was constructed at the U.S. Army Cold Regions Research and Engineering Laboratory in Hanover, New Hampshire, U.S.A. This bed was operated for the next three years using both anaerobically and aerobically digested sludges. Results indicate that both sludges were effectively dewatered by this process. The maximum depth of sludge frozen during this study was 1.14 m. The final solid contents were 39.3% and 24.5% for anaerobically digested and aerobically digested sludges respectively. The quality of the meltwater from the bed was similar to raw wastewater. The actual depth of sludge frozen and thawed in the bed during each year of operation was very close to that predicted by design models. Operational experience demonstrated the importance of a sand layer at the bottom of the bed for adequate drainage. Also, odors developed when the meltwater was allowed to accumulate in the bed. Odors were not a problem when the meltwater was drained away as quickly as it formed. Both sludges were easily removed with a front-end loader. Key words: sludge freezing bed, freeze–thaw conditioning, freeze–thaw separation, sludge dewatering, freezing bed.


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