Viewpoint: atmospheric CO2, soil water, and shrub/grass ratios on rangelands
Issue Date
1997-05-01Keywords
predictionplant ecology
water availability
soil water balance
carbon dioxide
atmosphere
greenhouse effect
stomata
C4 grasses
rain
transpiration
shrubs
rangelands
literature reviews
grasses
plant height
Metadata
Show full item recordCitation
Polley, H. W., Mayeux, H. S., Johnson, H. B., & Tischler, C. R. (1997). Atmospheric CO2, soil water, and shrub/grass ratios on rangelands. Journal of Range Management, 50(3), 278-284.Publisher
Society for Range ManagementJournal
Journal of Range ManagementDOI
10.2307/4003730Additional Links
https://rangelands.org/Abstract
The abundance of woody plants on grasslands and savannas often is controlled by the availability of water and its location in soil. Water availability to plants is limited by precipitation, but the distribution of soil water and period over which it is available in these ecosystems are influenced by the transpiration rates of grasses. We discuss implications of recent and projected increases in atmospheric CO2 concentration for transpiration, soil water availability, and the balance of grasses and shrubs. An increase in CO2 concentration often reduces potential transpiration/leaf area by reducing stomatal conductance. On grasslands where effects of stomatal closure on transpiration are not negated by an increase in leaf temperature and leaf area, rising CO2 concentration should slow the depletion of soil water by grasses and potentially favor shrubs and other species that might otherwise succumb to water stress. Predicted effects of CO2 are supported by results from CO2-enrichment studies in the field and are compatible with recent models of interactions between resource levels and vegetation pattern and structure.Type
textArticle
Language
enISSN
0022-409Xae974a485f413a2113503eed53cd6c53
10.2307/4003730