Full TGIF Record # 147050
Item 1 of 1
DOI:10.1016/j.agwat.2008.09.006
Web URL(s):http://www.sciencedirect.com/science/article/pii/S0378377408002096
    Last checked: 02/07/2014
    Access conditions: Item is within a limited-access website
Publication Type:
i
Refereed
Author(s):McCoy, E. L.; McCoy, K. R.
Author Affiliation:School of Environment and Natural Resources, Ohio Agricultural Research and Development Center, The Ohio State University, Wooster, Ohio
Title:Simulation of putting-green soil water dynamics: Implications for turfgrass water use
Source:Agricultural Water Management. Vol. 96, No. 3, March 2009, p. 405-414.
Publishing Information:[Amsterdam]: Elsevier Scientific Pub.
# of Pages:10
Keywords:TIC Keywords: Evapotranspiration; Irrigation; Permeability; Root zone mixture; Sand-based root zones; Soil water content; Soil water relations; USGA recommendations; Water uptake; Water use
Abstract/Contents:"Results from a field experiment examining soil water fate within U.S. Golf Association (USGA) putting greens were used to examine the validity of a water flow simulation model. The experiment used six different sandy root zones each with depths of 300 mm overlying a 100 mm thick gravel layer. Data collected over two growing seasons consisted of measured rainfall, irrigation, drainage volume, and soil water contents; and calculated turfgrass evapotranspiration (ET). Turfgrass rooting was measured at the end of each growing season, and water retention curve and saturated hydraulic conductivity measurements were conducted at the end of the study. For each root zone treatment, HYDRUS-2D (H2D) was calibrated using a subset of the experimental data and then validated by comparing observed and predicted water contents at 76, 152 and 229 mm depth and over both growing seasons. Model efficiency (E) ranged from 0.33 to 0.78; Mean Absolute Error (MAE) ranged from 0.012 to 0.024 m3 m-3; and Root Mean Square Error (RMSE) ranged from 0.015 to 0.028 m3 m-3, for the six treatments and both years. Also, RMSE values were at best slightly larger than and at worst twice as large as the mean standard deviation values of replicate measurements. Thus, H2D simulation performed reasonably well in describing the water content results of the field study. The calibration results provide evidence of hysteresis in water retention where water retention properties from the field appear to follow the sorption or wetting curve as compared with the laboratory measurements following the desorption or drying curve. This suggests that standard laboratory measurements of water release would not precisely predict water retention behavior in the field and over estimate water storage of these capillary barrier soils. The validation results provide evidence for turfgrass use of perched water held within these profiles, even though turfgrass rooting is shallow and water storage principally occurs deep within the root zone. Thus, the perched water of USGA putting greens should serve reasonably well as a water reservoir for subsequent turfgrass use, allowing for water conserving irrigation practices that makes use of this stored water."
Language:English
References:27
Note:Figures
Tables
Graphs
ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
McCoy, E. L., and K. R. McCoy. 2009. Simulation of putting-green soil water dynamics: Implications for turfgrass water use. Agric. Water Manage. 96(3):p. 405-414.
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DOI: 10.1016/j.agwat.2008.09.006
Web URL(s):
http://www.sciencedirect.com/science/article/pii/S0378377408002096
    Last checked: 02/07/2014
    Access conditions: Item is within a limited-access website
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MSU catalog number: b2205878a
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