1994
DOI: 10.1007/bf01416098
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Water relations, mineral nutrition, growth, and13C discrimination in two apple cultivars under daily episodes of high root-medium temperature

Abstract: Although high soil temperatures can occur in apple orchards throughout the world, there is little information on their effect. This investigation was conducted to determine the influence of various durations of root exposure to 34 °C on the growth and physiology of the apple plant. Roots of Royal Gala and McIntosh cultivhrs were exposed to 34 °C for 0, 8,16, and 24 hours/day for seven weeks. Royal Gala grown at the 24 hours/day treatment exhibited significant decreases in leaf, shoot, and root growth; chloroph… Show more

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Cited by 10 publications
(7 citation statements)
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“…Possible explanations of how root-zone temperature influenced C assimilation include an alteration in water uptake, modification of the endogenous plant growth regulator balance, or absorption of nutrients (Behboudian et al, 1994). Water uptake was altered in the present study with transpiration rates decreasing with supraoptimum (i.e., >25 °C) root-zone temperatures (data not shown).…”
Section: Discussionmentioning
confidence: 52%
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“…Possible explanations of how root-zone temperature influenced C assimilation include an alteration in water uptake, modification of the endogenous plant growth regulator balance, or absorption of nutrients (Behboudian et al, 1994). Water uptake was altered in the present study with transpiration rates decreasing with supraoptimum (i.e., >25 °C) root-zone temperatures (data not shown).…”
Section: Discussionmentioning
confidence: 52%
“…Water uptake was altered in the present study with transpiration rates decreasing with supraoptimum (i.e., >25 °C) root-zone temperatures (data not shown). This may have been a result of decreased levels of cytokinin-like substances in the roots and leaves (Gur et al, 1972) and also a possible increase in the synthesis of ABA resulting in stomatal closure (Behboudian et al, 1994). Other possible reasons for the root-zone temperature influence on net Pn include the mechanistic aspects of ion absorption and translocation (Natr, 1992).…”
Section: Discussionmentioning
confidence: 99%
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“…Thus, soil temperatures often covary with other microclimate parameters, and the independent effects of soil temperatures on plants are difficult to identify, particularly under natural conditions in the field. Supraoptimal soil temperatures caused water stress, reduced nutrient uptake, and lower photosynthesis in crops (BassiriRad et al ., 1991; Behboudian et al ., 1994; Udomprasert et al ., 1995; Dodd et al ., 2000; He et al ., 2001). Correlations of high soil temperature and reduced uptake of soil water at midsummer for woody species of south‐west North America (Lin et al ., 1996; Williams & Ehleringer, 2000) indicate that the significance of warm soils to native plants may be more important than is currently appreciated.…”
Section: Introductionmentioning
confidence: 99%
“…Increasing RZT from 25 to 30°C increases root-toshoot ratios (Awal et al, 2003) and can increase photosynthetic rates (Ziska, 1998). However, further increases in RZT can lead to growth inhibition by reducing nutrient uptake and chlorophyll content (Du and Tachibana, 1994), disturbing plant water relations and reducing g S (Behboudian et al, 1994) or altering plant chemical signaling (Dodd et al, 2000;Tachibana et al, 1997;Wang et al, 2004).…”
mentioning
confidence: 99%