scholarly journals Root Temperature Effects on Tuberous Root Growth of Sweetpotato (Ipomoea batatas Lam.). Direct and Indirect Effects of Temperature.

2003 ◽  
Vol 41 (1) ◽  
pp. 43-49 ◽  
Author(s):  
Toshihiko EGUCHI ◽  
Masaharu KITANO ◽  
Satoshi YOSHIDA ◽  
Jiro CHIKUSHI
1975 ◽  
Vol 5 (2) ◽  
pp. 171-175 ◽  
Author(s):  
Hugh E. Wilcox ◽  
Ruth Ganmore-Neumann

Seedlings of Pinusresinosa were grown at root temperatures of 16, 21 and 27 °C, both aseptically and after inoculation with the ectendomycorrhizal fungus BDG-58. Growth after 3 months was significantly influenced by the presence of the fungus at all 3 temperatures. The influence of the fungus on root growth was obscured by the effects of root temperature on morphology. The root system at 16 and at 21 °C possessed many first-order laterals with numerous, well developed second-order branches, but those at 27 °C had only a few, relatively long, unbranched first-order laterals. Although the root systems of infected seedlings were larger, the fungus increased root growth in the same pattern as determined by the temperature.


2017 ◽  
Vol 112 ◽  
pp. 110-116 ◽  
Author(s):  
Madeleine A. Rubenstein ◽  
Thomas W. Crowther ◽  
Daniel S. Maynard ◽  
Jonathan S. Schilling ◽  
Mark A. Bradford

2003 ◽  
Vol 48 (9) ◽  
pp. 145-154 ◽  
Author(s):  
J. German ◽  
G. Svensson ◽  
L.-G. Gustafsson ◽  
M. Vikström

The performance of stormwater ponds, operated under winter conditions, was modelled using the commercial software Mike21 and MOUSE. Direct and indirect effects of changing temperature were investigated. The most important effect of winter conditions is the changed hydrology, characterised by long periods with no runoff followed by snowmelt events with large runoff volumes during several days. This gives lower removal efficiencies than during a period with the same precipitation but without winter conditions. For the concentration of dissolved oxygen, wind is an important factor. Consequently the most important effect of an ice cover on the pond is that it prevents the oxygenation effects of the wind. The direct temperature effects on the removal processes are negligible compared to the indirect effects in changed hydrology and forming of ice cover.


2001 ◽  
Vol 79 (10) ◽  
pp. 1834-1841 ◽  
Author(s):  
Michael T. Anderson ◽  
Joseph M. Kiesecker ◽  
Douglas P. Chivers ◽  
Andrew R. Blaustein

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