SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 9 August 2007
Published in Soil Sci Soc Am J 71:1516-1523 (2007)
DOI: 10.2136/sssaj2006.0276
© 2007 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Hussein, J.
Right arrow Articles by Rose, C.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Hussein, J.
Right arrow Articles by Rose, C.
Agricola
Right arrow Articles by Hussein, J.
Right arrow Articles by Rose, C.
Related Collections
Right arrow Surface Water Quality
Right arrow Surface Hydrology
Right arrow Soil Erosion

SOIL & WATER MANAGEMENT & CONSERVATION

Sediment Retention by a Stiff Grass Hedge under Subcritical Flow Conditions

J. Husseina,*, H. Ghadiria, B. Yub and C. Rosec

a Australian Rivers Institute, Griffith Univ., 170 Kessels Rd, Nathan, QLD 4111, Australia
b Centre for Environmental Systems Research, Griffith Univ., 170 Kessels Rd, Nathan, QLD 4111, Australia
c Griffith School of Environment, Griffith Univ., 170 Kessels Rd, Nathan, QLD 4111, Australia

* Corresponding author (j.hussein{at}griffith.edu.au).

Reduction of diffuse fluxes of sediments from catchments is frequently achieved through the use of vegetative buffers, but the dynamics of this reduction are not fully understood. The physical processes involved in sediment deposition by a stiff grass buffer (hedge) at a low, subcritical flow rate were therefore examined. Flow experiments were performed in the Griffith University tilting-flume simulated rainfall facility using a 0.3-m-width, vetiver (Vetiveria zizaniodes L., sterile cultivar Monto) hedge at a 5% slope. Sediments comprising a sandy soil (Podzol) and red clay (Ferralsol) were introduced into the flow upstream of the buffer and the resultant hydrology, sediment deposition, and outflow characteristics were measured. Flow retardation produced a backwater upstream of the vetiver hedge and sediment deposition varied with soil type in this backwater. The backwater region was greatly extended by the deposition process, increasing overall sediment trapping efficiency. Buffering action reduced mean sediment loads in the outflow to 3.2 and 6.0% of the inflow concentration for the Podzol and Ferralsol, respectively, with a significant difference (P < 0.01) between the soils. In contrast to other buffer research where deposited sediments were coarsest upstream of the backwater, we found the coarsest particles at the downstream end for the Podzol and Ferralsol, indicating possible bed load movement in addition to the deposition and entrainment processes that dominate supercritical flow. The type of flow therefore affects the size distribution as well as the amount and efficiency of sediment deposition in front of vetiver hedges.

Abbreviations: GUTSR, Griffith University tilting-flume simulated rainfall facility • MWD, mean weight diameter







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 2007 by the Soil Science Society of America.