The role of transparent exopolymer particles (TEP) in the increase in apparent particle stickiness (α) during the decline of a diatom bloom

被引:189
作者
Engel, A [1 ]
机构
[1] Inst Meereskunde, D-24105 Kiel, Germany
关键词
D O I
10.1093/plankt/22.3.485
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
The termination of diatom spring blooms in temperate waters has been connected with the formation and subsequent rapid sedimentation of aggregates. According to coagulation theory, the rate of aggregate formation depends on the probability of particle collision and on the efficiency with which two particles adhere once they have collided (stickiness). During this study, the variation in particle stickiness was determined over the decline of a diatom bloom using the Couette Chamber assay with low shear (G = 0.86 s(-1)). A mixed diatom population, dominated by Skeletonema costatum, was sampled during the spring bloom in the Baltic Sea and incubated in the laboratory for 18 days. Measurements of diatom species composition, transparent exopolymer particles (TEP) and bulk particle abundance, as well as chemical and biological variables, were conducted in order to reveal the determinants of coagulation efficiency. The investigation showed that an increase in TEP concentration relative to conventional particles at the decline of the bloom significantly enhanced apparent coagulation efficiencies. High proportions of TEP led to apparent values of stickiness >1, which indicates that collision rates can be substantially underestimated when the stickiness parameter alpha is calculated on the basis of conventional particle counting only, e.g. with the Coulter Counter. A new stickiness parameter, alpha', was therefore estimated based on the combined volume fractions of TEP and conventional particles. The problems of stickiness measurements are discussed and the role of TEP in coagulation processes is emphasized.
引用
收藏
页码:485 / 497
页数:13
相关论文
共 44 条
[1]   THE ABUNDANCE AND SIGNIFICANCE OF A CLASS OF LARGE, TRANSPARENT ORGANIC PARTICLES IN THE OCEAN [J].
ALLDREDGE, AL ;
PASSOW, U ;
LOGAN, BE .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1993, 40 (06) :1131-1140
[2]   DIRECT OBSERVATIONS OF THE MASS FLOCCULATION OF DIATOM BLOOMS - CHARACTERISTICS, SETTLING VELOCITIES AND FORMATION OF DIATOM AGGREGATES [J].
ALLDREDGE, AL ;
GOTSCHALK, CC .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1989, 36 (02) :159-&
[3]   RAPID COUPLING OF SINKING PARTICLE FLUXES BETWEEN SURFACE AND DEEP OCEAN WATERS [J].
ASPER, VL ;
DEUSER, WG ;
KNAUER, GA ;
LOHRENZ, SE .
NATURE, 1992, 357 (6380) :670-672
[4]   ECOLOGY OF AMORPHOUS AGGREGATIONS (MARINE SNOW) IN THE NORTHERN ADRIATIC SEA .3. ZOOPLANKTON INTERACTIONS WITH MARINE SNOW [J].
BOCHDANSKY, AB ;
HERNDL, GJ .
MARINE ECOLOGY PROGRESS SERIES, 1992, 87 (1-2) :135-146
[5]   DIFFERENTIAL AGGREGATION OF DIATOMS [J].
CROCKER, KM ;
PASSOW, U .
MARINE ECOLOGY PROGRESS SERIES, 1995, 117 (1-3) :249-257
[6]   COAGULATION EFFICIENCY, ORGANIC-MATTER GLUES AND THE DYNAMICS OF PARTICLES DURING A PHYTOPLANKTON BLOOM IN A MESOCOSM STUDY [J].
DAM, HG ;
DRAPEAU, DT .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1995, 42 (01) :111-123
[7]   AN IMPROVED FLOCCULATOR DESIGN FOR USE IN PARTICLE AGGREGATION EXPERIMENTS [J].
DRAPEAU, DT ;
DAM, HG ;
GRENIER, G .
LIMNOLOGY AND OCEANOGRAPHY, 1994, 39 (03) :723-729
[8]   ROLE OF LARGE PARTICLES IN THE TRANSPORT OF ELEMENTS AND ORGANIC-COMPOUNDS THROUGH THE OCEANIC WATER COLUMN [J].
FOWLER, SW ;
KNAUER, GA .
PROGRESS IN OCEANOGRAPHY, 1986, 16 (03) :147-194
[9]  
Gardner W. D., 1997, OCEANOGRAPHY, V10, P116
[10]  
Grasshoff K., 1999, VERLAG CHEMIE FRG