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

Citation
Mc. Christie et al., Temporal and spatial distributions of moisture and organic contents acrossa macro-tidal mudflat, CONT SHELF, 20(10-11), 2000, pp. 1219-1241
Citations number
20
Categorie Soggetti
Aquatic Sciences
Journal title
CONTINENTAL SHELF RESEARCH
ISSN journal
02784343 → ACNP
Volume
20
Issue
10-11
Year of publication
2000
Pages
1219 - 1241
Database
ISI
SICI code
0278-4343(200007/08)20:10-11<1219:TASDOM>2.0.ZU;2-
Abstract
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 o n the sediment properties. Sediment cores were collected using modified 50 mi syringes, and the data compared with measurements of chlorophyll a and c olloidal carbohydrate concentrations. The temporal and spatial relationship s between these surface sediment properties were quantified and related to the measured critical erosion shear stress. Moisture and organic contents c orrelate significantly with respect to morphology, both across the mudflat and with depth below the sediment surface, These variations affected the di stributions of bulk density and sediment erodibility, although these two va riables were not directly related. The relatively coarse vertical resolutio n of the cores prevented clear relationships being identified between criti cal erosion shear stress, moisture and organic contents, and the chlorophyl l a and colloidal carbohydrate concentrations. Analysis of mean values remo ved some of the spatial variability and a reasonable exponential relationsh ip was obtained between erosion shear stress and colloidal carbohydrate. Th is paper highlights the influence of the physical, morphological and biolog ical characteristics of the surface sediment upon its erosion resistance. T he implications for the development of the surface morphology and mudflat a re considered. (C) 2000 Elsevier Science Ltd. All rights reserved.