Influence of transparent exopolymer particles (TEP) on sinking velocity of Nitzschia closterium aggregates

被引:88
作者
Engel, A [1 ]
Schartau, M [1 ]
机构
[1] Univ Kiel, Inst Meereskunde Kiel, D-24105 Kiel, Germany
关键词
phytoplankton; aggregates; TEP; Nitzschia closterium; sinking velocity; fractal dimension;
D O I
10.3354/meps182069
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Sinking velocities of more than 300 Nitzschia closterium aggregates were determined during roller table incubation using digital image analysis. To examine the influence of transparent exopolymer particles (TEP) on aggregate settling speed, 3 experiments with different ratios of TEP to cell volume concentration were conducted. The results showed that, for N, closterium aggregates without TEP, sinking velocity (U) was significantly related to the equivalent spherical diameter (ESD) of the aggregates, yielding U (cm s(-1)) = 1.89 (ESD, cm)(0.55). The higher was the specific TEP content of an aggregate, the lower was the sinking velocity and the less pronounced was the size versus velocity relationship. Excess densities (Delta rho) of aggregates were derived from velocity measurements and 3-dimensional fractal dimensions (D3) of aggregates were calculated from scaling properties of Delta rho. Values for D3 never exceeded 2 and fit well to Values of the 2-dimensional fractal dimension (D2) attained from image analysis.
引用
收藏
页码:69 / 76
页数:8
相关论文
共 41 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]   INSITU SETTLING BEHAVIOR OF MARINE SNOW [J].
ALLDREDGE, AL ;
GOTSCHALK, C .
LIMNOLOGY AND OCEANOGRAPHY, 1988, 33 (03) :339-351
[3]   WHY DO SINKING MUCILAGE AGGREGATES ACCUMULATE IN THE WATER COLUMN [J].
ALLDREDGE, AL ;
CROCKER, KM .
SCIENCE OF THE TOTAL ENVIRONMENT, 1995, 165 (1-3) :15-22
[4]   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-&
[5]   CHARACTERISTICS, DYNAMICS AND SIGNIFICANCE OF MARINE SNOW [J].
ALLDREDGE, AL ;
SILVER, MW .
PROGRESS IN OCEANOGRAPHY, 1988, 20 (01) :41-82
[6]   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
[7]  
CABRINI M, 1992, SCI TOT ENV SUPPL, P557
[8]   FRACTAL GEOMETRY OF IN-SITU FLOCS IN THE ESTUARINE AND COASTAL ENVIRONMENTS [J].
CHEN, SM ;
EISMA, D .
NETHERLANDS JOURNAL OF SEA RESEARCH, 1995, 33 (02) :173-182
[9]   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
[10]   In situ settling speeds of marine snow aggregates below the mixed layer: Black Sea and Gulf of Mexico [J].
Diercks, AR ;
Asper, VL .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1997, 44 (03) :385-&