Embryonic development and effect of water temperature on hatching of Lophius litulon

Author(s):  
Tomoya Ishikawa ◽  
Mitsuhiro Nakaya ◽  
Tetsuya Takatsu
2016 ◽  
Vol 32 (1) ◽  
pp. 37-43
Author(s):  
Sin-Kil Kang ◽  
Chan-Gyoung Sung ◽  
Jiwoong Chung ◽  
Dong-Ho Park ◽  
Jong-Hyeon Lee ◽  
...  

Aquaculture ◽  
2012 ◽  
Vol 330-333 ◽  
pp. 100-105 ◽  
Author(s):  
Hyojin Ahn ◽  
Yoshiaki Yamada ◽  
Akihiro Okamura ◽  
Noriyuki Horie ◽  
Naomi Mikawa ◽  
...  

2020 ◽  
Vol 32 (2) ◽  
pp. 78-83
Author(s):  
Jin Choi ◽  
Gyeong Sik Han ◽  
Ki Wook Lee ◽  
Soon-Gyu Byun ◽  
Hyun Jeong Lim ◽  
...  

2021 ◽  
pp. 101836
Author(s):  
Kodama Saki ◽  
Hata Junichi ◽  
Kanawaku Yoshimasa ◽  
Nakagawa Hiroshi ◽  
Oshiro Hinako ◽  
...  

Author(s):  
R.A. Cooper ◽  
Bryany Hill ◽  
J.A. Kirk

It is commonly held that goats prefer their water ‘warm’ and that consumption may be encouraged by offering warmed water. Conversely, it is argued that water intake may go down if water is ‘too cold.’ There are, however, few data available and no definition of what constitutes ‘warm’ or ‘cold’ in the eyes of a goat. This trial was undertaken to provide some data in an attempt to confirm or refuse these conventional wisdoms.


2016 ◽  
Vol 48 (4) ◽  
pp. 1877-1884 ◽  
Author(s):  
Jan Matousek ◽  
Vlastimil Stejskal ◽  
Marketa Prokesova ◽  
Jan Kouril

2013 ◽  
Vol 45 (1) ◽  
pp. 89-98 ◽  
Author(s):  
Weihong Dong ◽  
Gengxin Ou ◽  
Xunhong Chen ◽  
Zhaowei Wang

In this study, in situ and on-site permeameter tests were conducted in Clear Creek, Nebraska, USA to evaluate the effect of water temperature on streambed vertical hydraulic conductivity Kv. Fifty-two sediment cores were tested. Five of them were transferred to the laboratory for a series of experiments to evaluate the effect of water temperature on Kv. Compared with in situ tests, 42 out of the 52 tests have higher Kv values for on-site tests. The distribution of water temperature at the approximately 50 cm depth of streambed along the sand bar was investigated in the field. These temperatures had values in the range 14–19 °C with an average of 16 °C and had an increasing trend along the stream flow. On average, Kv values of the streambed sediments in the laboratory tests increase by 1.8% per 1 °C increase in water temperature. The coarser sandy sediments show a greater increase extent of the Kv value per 1 °C increase in water temperature. However, there is no distinct increasing trend of Kv value for sediment containing silt and clay layers.


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