Transpiration and visual appearance of warm season turfgrasses during soil drying |
| |
| Institution: | 1. Department of Environmental Horticulture, University of Florida, P.O. Box 110670, Gainesville, FL 32611-0670, United States;2. Department of Crop Science, North Carolina State University, Campus Box 7620, Raleigh, NC 27695-7620, United States;3. Department of Agricultural and Biological Engineering, P.O. Box 110570, Gainesville, FL 32611-0570, United States;1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China;1. Bioforsk – Norwegian Institute for Agricultural and Environmental Research, Landvik, 4886 Grimstad, Norway;2. Bioforsk – Norwegian Institute for Agricultural and Environmental Research Særheim, 4353 Klepp, Norway;1. Division of Plastic Surgery, Baylor College of Medicine, United States;2. Department of Radiology, Texas Children''s Hospital, United States;3. Department of Otolaryngology, Texas Children''s Hospital, 6550 Fannin St., Suite 2001, Houston, TX 77030, United States;1. Ookusa Animal Clinic, Ookusa 503, Matsue, Shimane 690-0032, Japan;2. Dian Fossey Gorilla Fund International, Atlanta, USA;3. Department of Environmental Sciences and Environmental Health, Emory University and Rollins School of Public Health, Atlanta, USA;4. Division of Pathobiological Analysis, Department of Veterinary Pathobiology, School of Veterinary Medicine, Nippon Veterinary and Life Science University, Tokyo, Japan;1. University of Agriculture in Kraków, Faculty of Agriculture and Economics, Department of Plant Physiology, Pod?u?na 3, 30-239 Kraków, Poland;2. The Franciszek Górski Institute of Plant Physiology, Polish Academy of Sciences, Niezapominajek 21, 30-239 Kraków, Poland;1. National Agriculture and Food Research Organization Tohoku Agricultural Research Center, 50 Harajukuminami, Arai, Fukushima-shi, Fukushima 960-2156, Japan;2. Fukushima Agricultural Technology Centre, 116 Shimonakamichi, Takakura-Aza, Hiwada-machi, Koriyama, Fukushima 963-0531, Japan |
| |
| Abstract: | Warm-season turfgrasses may be subjected to increasing drought as future urban irrigation regulations become more restrictive. Species differences in water use and transpiration response to drying soil may be exploited in the future to increase survival and maintain green color under drying soil conditions. This study was undertaken to provide background documentation on the sensitivity to soil–water deficit of three warm-season grasses: ‘Argentine’ bahiagrass (Paspalum notatum); ‘Floratam’ St. Augustinegrass (Stenotaphrum secundatum), and ‘Empire’ zoysiagrass (Zoysia japonica). Each of these turfgrasses demonstrated a two-phased linear transpiration response to gradually drying soil as expressed by a normalized ratio between the transpiration rates of drought stressed to well-watered plants (NTR). In this study, well-watered bahiagrass used 30% more water on a daily basis than did well-watered St. Augustinegrass or zoysiagrass. However, under drought, the three grass species transpired the same amount of water during the soil drying period up until NTR to 0.1. Since bahiagrass reached an NTR of 0.1 at 10.3 days versus 12.7 and 13.0 days for St. Augustinegrass and zoysiagrass, respectively, bahiagrass demonstrated a more rapid water loss rate during the drying period. The fraction of transpirable soil water (FTSW) remaining in the soil at the breakpoints for bahiagrass, St. Augustinegrass and zoysiagrass were 0.13, 0.16, and 0.19, respectively, in 2010, but were 0.18, 0.30, and 0.22, respectively, under slightly warmer conditions in 2011. The consistently low FTSW breakpoint for bahiagrass means that compared to the other species, bahiagrass continues to use water at a high rate late into the soil drying cycle before conserving soil water by decreasing stomatal conductance. That is, bahiagrass is likely to be subjected to greater soil–water deficits in lengthy droughts and needs mechanisms to better survive these droughts. The differences in breakpoints by year may be due to a combination of soil factors and temperature differences in the greenhouse. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
