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-List Of Titles -Fine root biomass and its relationship to evapotranspiration in woody and grassy vegetation covers for ecological restoration of waste storage and mining landscapes

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/178283

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Title
Fine root biomass and its relationship to evapotranspiration in woody and grassy vegetation covers for ecological restoration of waste storage and mining landscapes
Related
Ecosystems, Vol. 15, No. 1, (2012), p.113-127
DOI
10.1007/s10021-011-9496-9
Publisher
Springer
Date
2012
Author/Creator
Yunusa, Isa A. M
Author/Creator
Zolfaghar, Sepideh
Author/Creator
Zeppel, Melanie J. B
Author/Creator
Li, Zheng
Author/Creator
Palmer, Anthony R
Author/Creator
Eamus, Derek
Description
Production and distribution of fine roots (≤2.0 mm diameter) are central to belowground ecological processes. This is especially true where vegetation serves as a pump to prevent saturation of soil and possible drainage of excess water into or from potentially toxic waste material stored underground or in mounds aboveground. In this study undertaken near Sydney in Australia, we determined fine root biomass and evapotranspiration (ET) on a waste disposal site restored with either a 15-year-old grass sward or plantations of mixed woody species that were either 5 years old (plantation-5) with a vigorous groundcover of pasture legumes and grasses, or 3 years old (plantation-3) with sparse groundcover. These sites were compared with nearby remnant woodland; all four were located within 0.5-km radius at the same site. Ranking of fine root biomass was in the order woodland (12.3 Mg ha⁻¹) > plantation-5 (8.3 Mg ha⁻¹) > grass (4.9 Mg ha⁻¹) > plantation-3 (1.2 Mg ha⁻¹) and was not correlated with nutrient contents in soil or plants, but reflected the form and age of the vegetation covers. Trends in root length density (RLD) and root area index (RAI) followed those in root biomass, but the differences in RAI were larger than those in biomass amongst the vegetation covers. Annual ET in the dry year of 2009 was similar in the three woody vegetation covers (652–683 mm) and was at least 15% larger than for the grass (555 mm), which experienced restrained growth in winter and periodic mowing. This resulted in drainage from the grass cover while there was no drainage from any of the woody vegetation covers. In plantation-5, root biomass, RAI and RLD were reduced in the rain shadow side of the tree rows. Similarly, the amount and depth of rooting in the groundcover were reduced close to the trees compared to midway between rows. Differences in the root variables were larger than those in ET, which suggested that more roots were produced than were needed for water uptake and/or presence of considerable amounts of necromass. We conclude that vegetation covers, such as plantation-5 consisting of widely spaced trees and a heavy groundcover containing winter-active pasture legumes, will promote year-round water-use with a reduced risk of deep rooting that could breach buried wastes. This function could be sustained through progressive thinning of trees to account for not more than 25% of the whole canopy cover; this will minimize competition for limited soil-water and thereby constrain deep rooting as vegetation ages and attains climax.
Description
15 page(s)
Subject Keyword
Drainage
Subject Keyword
ecological restoration
Subject Keyword
evapotranspiration
Subject Keyword
land degradation
Subject Keyword
root area index
Subject Keyword
root biomass
Subject Keyword
root length density
Subject Keyword
waste disposal
Resource Type
journal article
Organisation
Macquarie University. Dept. of Biological Sciences

Identifier
http://hdl.handle.net/1959.14/178283
Identifier
ISSN:1432-9840
Identifier
mq_res-ext-2-s2.0-84856530223
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Ecosystems"
 
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