学术探索
学术期刊
学术作者
新闻热点
数据分析
智能评审

CHARACTERISTICS OF ALGINATE FROM LAMINARIA-DIGITATA CULTIVATED IN A HIGH-PHOSPHATE ENVIRONMENT

被引：35
作者：
INDERGAARD, M
SKJAKBRAEK, G
机构：
来源：
HYDROBIOLOGIA | 1987年 / 151卷
关键词：
D O I：
10.1007/BF00046180
中图分类号：
Q17 [水生生物学];
学科分类号：
071004 [水生生物学];
摘要：
引用
收藏
页码：541 / 549
页数：9
相关论文
共 31 条
[1]
BIDWELL RGS, 1982, SYNTHETIC DEGRADATIV, P237
[2]
THE SEASONAL VARIATION IN CHEMICAL CONSTITUTION OF SOME OF THE SUBLITTORAL SEAWEEDS COMMON TO SCOTLAND .3. LAMINARIA-SACCHARINA AND SACCORHIZA-BULBOSA [J].
BLACK, WAP .
JOURNAL OF THE SOCIETY OF CHEMICAL INDUSTRY-LONDON, 1948, 67 (05) :172-176
[3]
SEASONAL GROWTH IN LAMINARIA-LONGICRURIS - RELATIONS WITH DISSOLVED INORGANIC NUTRIENTS AND INTERNAL RESERVES OF NITROGEN [J].
CHAPMAN, ARO ;
CRAIGIE, JS .
MARINE BIOLOGY, 1977, 40 (03) :197-205
[4]
SEASONAL GROWTH IN LAMINARIA-LONGICRURIS - RELATIONS WITH RESERVE CARBOHYDRATE STORAGE AND PRODUCTION [J].
CHAPMAN, ARO ;
CRAIGIE, JS .
MARINE BIOLOGY, 1978, 46 (03) :209-213
[5]
THE ENVIRONMENTAL-ROLE OF ALGINATES IN DURVILLAEA-POTATORUM (FUCALES, PHAEOPHYTA) [J].
CHESHIRE, AC ;
HALLAM, ND .
PHYCOLOGIA, 1985, 24 (02) :147-153
[6]
INTERSPECIFIC, INTRASPECIFIC AND NUTRITIONALLY-DETERMINED VARIATIONS IN THE COMPOSITION OF AGARS FROM GRACILARIA SPP [J].
CRAIGIE, JS ;
WEN, ZC ;
VANDERMEER, JP .
BOTANICA MARINA, 1984, 27 (02) :55-61
[7]
ALGINATE BLOCK STRUCTURE IN PHAEOPHYCEAE FROM NOVA-SCOTIA - VARIATION WITH SPECIES, ENVIRONMENT AND TISSUE-TYPE [J].
CRAIGIE, JS ;
MORRIS, ER ;
REES, DA ;
THOM, D .
CARBOHYDRATE POLYMERS, 1984, 4 (04) :237-252
[8]
PMR STUDY OF THE COMPOSITION AND SEQUENCE OF URONATE RESIDUES IN ALGINATES [J].
GRASDALEN, H ;
LARSEN, B ;
SMIDSROD, O .
CARBOHYDRATE RESEARCH, 1979, 68 (01) :23-31
[9]
HIGH-FIELD, H-1-NMR SPECTROSCOPY OF ALGINATE - SEQUENTIAL STRUCTURE AND LINKAGE CONFORMATIONS [J].
GRASDALEN, H .
CARBOHYDRATE RESEARCH, 1983, 118 (JUL) :255-260
[10]
URONIC ACID SEQUENCE IN ALGINATE FROM DIFFERENT SOURCES [J].
HAUG, A ;
LARSEN, B ;
SMIDSROD, O .
CARBOHYDRATE RESEARCH, 1974, 32 (02) :217-225
1234