The impact of recrystallisation on the freeze‐thaw cycles of red seabream (
            Pagrus major
            ) fillets

Freeze–thaw action is considered to be one of the most destructive actions that can induce significant damage in stabilized subgrades in seasonally frozen loess areas. Laboratory tests including frost heave – thaw shrinkage and microstructure change during freeze–thaw cycles were conducted to evaluate the volume change rate of loess stabilized with cement, lime, and fly ash under the impact of cyclic freeze–thaw conditions. The loess specimens collapsed after eight freeze–thaw cycles (192 h), but most stabilized loess specimens had no visible damage after all freeze–thaw cycles were completed. All of the stabilized loess samples underwent a much smaller volume change than the loess alone after the freeze–thaw cycles. Although surface porosity and equivalent diameter of stabilized loess samples increased, the stabilized loess can retain its microstructure during freeze–thaw cycles when the cement content was less than 6%. To ensure freeze–thaw resistance of stabilized loess subgrades, the mix proportions of the three additives was recommended to be 4 to 5% cement, 6% lime, and 10% fly ash.

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Central distribution of kiss2 neurons and peri-pubertal changes in their expression in the brain of male and female red seabream Pagrus major

General and Comparative Endocrinology ◽

10.1016/j.ygcen.2011.11.038 ◽

2012 ◽

Vol 175 (3) ◽

pp. 432-442 ◽

Cited By ~ 23

Author(s):

Yuki Shimizu ◽

Junko Tomikawa ◽

Keisuke Hirano ◽

Yoko Nanikawa ◽

Yasuhisa Akazome ◽

...

Keyword(s):

Pagrus Major ◽

Male And Female ◽

Red Seabream ◽

The Brain

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The Impact of Freeze–thaw on the Stability of Soil Cut Slope in High-latitude Frozen Regions

Landslides in Cold Regions in the Context of Climate Change - Environmental Science and Engineering ◽

10.1007/978-3-319-00867-7_7 ◽

2013 ◽

pp. 85-98 ◽

Cited By ~ 1

Author(s):

Ying Guo ◽

Wei Shan ◽

Hua Jiang ◽

Yuying Sun ◽

Chengcheng Zhang

Keyword(s):

High Latitude ◽

Cut Slope ◽

Freeze Thaw ◽

The Stability ◽

The Impact

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Long-term stability of RNA isolated from muscle of red seabream (Pagrus major) during ice storage

Fish Physiology and Biochemistry ◽

10.1007/s10695-018-0588-8 ◽

2018 ◽

Vol 45 (2) ◽

pp. 819-828

Author(s):

Nobuyoshi Nakatsuji ◽

Kohsuke Adachi ◽

Katsuji Morioka

Keyword(s):

Ice Storage ◽

Pagrus Major ◽

Red Seabream ◽

Term Stability ◽

Long Term Stability

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Effects of feeding on the growth and survival of red seabream larval Pagrus major.

Tropical Oceanography ◽

10.5914/tropocean.v21i1.2650 ◽

1990 ◽

Vol 21 (1) ◽

Author(s):

Sérgio Macedo Gomes de MATTOS ◽

Márcia Santos Nunes GALVÃO

Keyword(s):

Pagrus Major ◽

Growth And Survival ◽

Red Seabream

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USING SMOS PASSIVE MICROWAVE DATA TO DEVELOP SMAP FREEZE/THAW ALGORITHMS ADAPTED FOR THE CANADIAN SUBARCTIC

ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences ◽

10.5194/isprsarchives-xl-1-w5-365-2015 ◽

2015 ◽

Vol XL-1-W5 ◽

pp. 365-368 ◽

Cited By ~ 1

Author(s):

P. Kalantari ◽

M. Bernier ◽

K. C. McDonal ◽

J. Poulin

Keyword(s):

Land Cover ◽

Time Series Data ◽

Passive Microwave ◽

Soil Freezing ◽

Series Data ◽

Freezing And Thawing ◽

Freeze Thaw ◽

Thaw Cycle ◽

Freeze Thaw Cycle ◽

The Impact

Seasonal terrestrial Freeze/Thaw cycle in Northern Quebec Tundra (Nunavik) was determined and evaluated with passive microwave observations. SMOS time series data were analyzed to examine seasonal variations of soil freezing, and to assess the impact of land cover on the Freeze/Thaw cycle. Furthermore, the soil freezing maps derived from SMOS observations were compared to field survey data in the region near Umiujaq. The objective is to develop algorithms to follow the seasonal cycle of freezing and thawing of the soil adapted to Canadian subarctic, a territory with a high complexity of land cover (vegetation, soil, and water bodies). Field data shows that soil freezing and thawing dates vary much spatially at the local scale in the Boreal Forest and the Tundra. The results showed a satisfactory pixel by pixel mapping for the daily soil state monitoring with a > 80% success rate with in situ data for the HH and VV polarizations, and for different land cover. The average accuracies are 80% and 84% for the soil freeze period, and soil thaw period respectively. The comparison is limited because of the small number of validation pixels.

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