Temporal and spatial distributions of moisture and organic contents across a macro-tidal mudflat

被引:29
作者
Christie, MC [1 ]
Dyer, KR
Blanchard, G
Cramp, A
Mitchener, HJ
Paterson, DM
机构
[1] Univ Plymouth, Inst Marine Studies, Plymouth PL4 8AA, Devon, England
[2] Ctr Rech Ecol Marine & Aquaculture Houmeau, F-17137 Houmeau, France
[3] Cardiff Univ, Dept Earth Sci, Cardiff CF1 3YE, S Glam, Wales
[4] HR Wallingford Ltd, Marine Sediments Res Grp, Wallingford OX10 8BA, Oxon, England
[5] Univ St Andrews, Gatty Marine Lab, Sch Environm & Evolut Biol, Sediment Ecol Res Grp, St Andrews KY16 8LB, Fife, Scotland
关键词
mudflats; moisture; organic matter; carbohydrate; erosion; Humber estuary;
D O I
10.1016/S0278-4343(00)00020-0
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The purpose of this study was to make comprehensive surface measurements of the changes in moisture and organic contents across the Skeffling mudflats (Humber Estuary, UK) and to examine the effects of exposure and location on the sediment properties. Sediment cores were collected using modified 50 mi syringes, and the data compared with measurements of chlorophyll a and colloidal carbohydrate concentrations. The temporal and spatial relationships between these surface sediment properties were quantified and related to the measured critical erosion shear stress. Moisture and organic contents correlate significantly with respect to morphology, both across the mudflat and with depth below the sediment surface, These variations affected the distributions of bulk density and sediment erodibility, although these two variables were not directly related. The relatively coarse vertical resolution of the cores prevented clear relationships being identified between critical erosion shear stress, moisture and organic contents, and the chlorophyll a and colloidal carbohydrate concentrations. Analysis of mean values removed some of the spatial variability and a reasonable exponential relationship was obtained between erosion shear stress and colloidal carbohydrate. This paper highlights the influence of the physical, morphological and biological characteristics of the surface sediment upon its erosion resistance. The implications for the development of the surface morphology and mudflat are considered. (C) 2000 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:1219 / 1241
页数:23
相关论文
共 20 条
[1]  
BLACK KS, 1998, SPECIAL PUBLICATION, V139, P45
[2]   The effect of geomorphological structures on potential biostabilisation by microphytobenthos on intertidal mudflats [J].
Blanchard, GF ;
Paterson, DM ;
Stal, LJ ;
Richard, P ;
Galois, R ;
Huet, V ;
Kelly, J ;
Honeywill, C ;
de Brouwer, J ;
Dyer, K ;
Christie, M ;
Seguignes, M .
CONTINENTAL SHELF RESEARCH, 2000, 20 (10-11) :1243-1256
[3]  
Christie MC, 1998, GEOL SOC SPEC PUBL, V139, P45, DOI 10.1144/GSL.SP.1998.139.01.04
[4]   Sediment flux and bed level measurements from a macro tidal mudflat [J].
Christie, MC ;
Dyer, KR ;
Turner, P .
ESTUARINE COASTAL AND SHELF SCIENCE, 1999, 49 (05) :667-688
[5]   Interplay between biology and sedimentology in a mudflat (Biezelingse Ham, Westerschelde, The Netherlands) [J].
de Brouwer, JFC ;
Bjelic, S ;
de Deckere, EMGT ;
Stal, LJ .
CONTINENTAL SHELF RESEARCH, 2000, 20 (10-11) :1159-1177
[6]  
Decho A. W., 1994, BIOSTABILIZATION SED, P135
[7]  
Edgar LA., 1984, PROG PHYCOL RES, V3, P47
[8]   Erosion of mud/sand mixtures [J].
Mitchener, H ;
Torfs, H .
COASTAL ENGINEERING, 1996, 29 (1-2) :1-25
[9]   Erosion of mud/sand mixtures (vol 29, pg 1, 1996) [J].
Mitchener, H ;
Torfs, H ;
Whitehouse, R .
COASTAL ENGINEERING, 1997, 30 (3-4) :319-319
[10]  
MITCHENER HJ, 1998, 52 TR HR WALL