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Journal ArticleDOI

A global analysis of root distributions for terrestrial biomes

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TLDR
Rooting patterns for terrestrial biomes are analyzed and distributions for various plant functional groups are compared and the merits and possible shortcomings of the analysis are discussed in the context of root biomass and root functioning.
Abstract
Understanding and predicting ecosystem functioning (e.g., carbon and water fluxes) and the role of soils in carbon storage requires an accurate assessment of plant rooting distributions. Here, in a comprehensive literature synthesis, we analyze rooting patterns for terrestrial biomes and compare distributions for various plant functional groups. We compiled a database of 250 root studies, subdividing suitable results into 11 biomes, and fitted the depth coefficient β to the data for each biome (Gale and Grigal 1987). β is a simple numerical index of rooting distribution based on the asymptotic equation Y=1-βd, where d = depth and Y = the proportion of roots from the surface to depth d. High values of β correspond to a greater proportion of roots with depth. Tundra, boreal forest, and temperate grasslands showed the shallowest rooting profiles (β=0.913, 0.943, and 0.943, respectively), with 80-90% of roots in the top 30 cm of soil; deserts and temperate coniferous forests showed the deepest profiles (β=0.975 and 0.976, respectively) and had only 50% of their roots in the upper 30 cm. Standing root biomass varied by over an order of magnitude across biomes, from approximately 0.2 to 5 kg m-2. Tropical evergreen forests had the highest root biomass (5 kg m-2), but other forest biomes and sclerophyllous shrublands were of similar magnitude. Root biomass for croplands, deserts, tundra and grasslands was below 1.5 kg m-2. Root/shoot (R/S) ratios were highest for tundra, grasslands, and cold deserts (ranging from 4 to 7); forest ecosystems and croplands had the lowest R/S ratios (approximately 0.1 to 0.5). Comparing data across biomes for plant functional groups, grasses had 44% of their roots in the top 10 cm of soil. (β=0.952), while shrubs had only 21% in the same depth increment (β=0.978). The rooting distribution of all temperate and tropical trees was β=0.970 with 26% of roots in the top 10 cm and 60% in the top 30 cm. Overall, the globally averaged root distribution for all ecosystems was β=0.966 (r 2=0.89) with approximately 30%, 50%, and 75% of roots in the top 10 cm, 20 cm, and 40 cm, respectively. We discuss the merits and possible shortcomings of our analysis in the context of root biomass and root functioning.

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Investigating soil moisture-climate interactions in a changing climate: A review

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References
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Journal ArticleDOI

Water losses in the Patagonian steppe: A modelling approach

TL;DR: In this paper, the authors developed a soil water model for the Patagonian steppe with a daily time step, which gives weekly cumulative values of transpiration, evaporation, and drainage, maximum and minimum water content for the different soil layers in each week, and the weekly fre- quency of days with soil water potential higher than -1 MPa for each layer.
Journal ArticleDOI

Plant Biomass and Productivity of Prairie, Savanna, Oakwood, and Maize Field Ecosystems in Central Minnesota

TL;DR: The Cedar Creek Natural History Area is located 50 km (30 mi) north of Minneapolis and St. Paul, Minnesota, and is about 1,620 hectares (4,000 acres) in area.
Journal ArticleDOI

Three-dimensional distribution of plant biomass in relation to grazing and topography in the shortgrass steppe

Daniel G. Milchunas, +1 more
- 01 May 1989 - 
TL;DR: The grazing-lawn concept is extended to the belowground plant community and discussed in terms of possible herbivore mediated plant-plant interactions rather than as an aboveground grazing avoidance mechanism.
Journal ArticleDOI

Relations between mineral nutrient availability and fine root biomass in two Costa Rican tropical wet forests: a hypothesis.

Stith T. Gower
- 01 Jun 1987 - 
TL;DR: Fine root biomass was estimated for two Costa Rican broad-leaf evergreen forests with apparent differences in soil nutrient status and the amount of freezer space available at the La Selva Research Station, and the lack of data on weatherable mineral content.
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