1) sea ice bacterium
海冰细菌
1.
Preliminary study on low-temperature adaptation of Antarctic sea ice bacterium Colwellia sp.;
南极海冰细菌科尔韦尔氏菌低温适应性的初步研究
2) ice nucleation active bacteria
冰核细菌
1.
Dynamic changes of ice nucleation active bacterial population inhabiting on corn in Northern China;
冰核细菌在我国北方玉米上的消长动态规律
2.
The biological characteristics,safety and application in food industry of ice nucleation active bacteria were summarized in this paper, moreover,its development in the future was also discussed.
对冰核细菌的生物学特性、安全性及其在食品冷冻保鲜与冷冻浓缩中的应用进行了概述,并对其今后在食品工业中的应用前景进行了展望。
3.
The paper summarizes the recent progress in studies on cold resistance of fruit tree, including the methods in study of cold resistance, the correlation between tissue structure of organs and chilling requirement with cold resistance, the study of ice nucleation active bacteria.
本文对果树抗寒性的研究鉴定方法,器官组织结构、需寒量与抗寒性的相关性,冰核细菌的研究进展,及在越冬前寒冷驯化中植物细胞的生理变化进行了较系统的综述。
3) INA bacteria
冰核细菌
1.
In 1974,Maki first reported ice nucleation active bacteria (INA bacteria).
自 1 974年 ,Maki首次报道了冰核细菌 ( INA细菌 )以来 ,生物冰核现象引起了多个学科研究者的广泛兴趣。
2.
s:Sixty strains of ice nucleation active bacteria(INA bacteria) were isolated on 25 kinds of plants in Shandong province.
这是山东省关于冰核细菌研究的首次报道。
3.
Objective: To verificate that INA bacteria is an important factor that induce and increase banana freezing injury through the artificial climate chamber simulation test; To obtain a kind of highly effective and lowly toxic anti-frost Pharmacy through INA bacteria inhibitory, killing, and destroying experiments.
目的:通过人工模拟气候室试验,验证冰核细菌是诱发和加重香蕉霜冻害的一个重要因素。
4) bacterial ice nucleators
细菌冰核
5) ice bacteriology
冰细菌学
6) marine bacteria
海洋细菌
1.
Effect of nutrients on marine bacteria for their growth and the degradation of petroleum hydrocarbon;
营养盐对湄洲湾海洋细菌生长及降解石油烃的影响
2.
Methods of fluorescence enumeration of marine bacteria and application;
海洋细菌荧光显微计数法及其应用
3.
Adhesion of marine bacteria on three antifouling coatings based on waterborne polyurethane;
水性聚氨酯防污涂料的海洋细菌附着实验
补充资料:海冰
海冰 sea ice 海洋中冻结而成的咸水冰 。广义的海冰还包括在海洋中的河冰、冰山等。最初形成的海冰是针状的或薄片状的,随后聚集和凝结,并在风力、海流、海浪和潮汐的作用下,互相堆叠而成重叠冰和堆积冰。一般情况下都浮于海面,形状规则的海冰露出水面的高度为总厚度的1/7~1/10,尖顶冰露出的高度达总厚度的 1/4~1/3。反射率为0.50~0.70,抗压强度约为淡水冰的3/4。海冰可分为两类:①固定冰。多分布在大陆沿岸或岛屿附近,与海岸、岛屿,甚至与海底冻结在一起。②浮冰或冰山。随风、浪、流而漂移。 海冰在极地的分布具有显著的季节性变化和年际变化。①北半球。冰界以3~4月最大,8~9月最小。北冰洋几乎全为冰所覆盖,流冰群主要绕洋盆边缘流动,多为3~4米厚的多年冰。②南半球。多为2~3米厚的、到了夏天就能融化的冰,大致呈纬向分布,冰区以9月(属冬天)最大,3月(属夏天)最小。固定冰分布南极大陆周围和威德尔海。浮冰冰界在南太平洋、南印度洋和南大西洋。分别在南纬50°~55°、南纬45°~55°和南纬43°~55°。 |
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条