The combined effect of water status and crop level on Tempranillo wine volatiles

2016 ◽  
Vol 97 (5) ◽  
pp. 1533-1542 ◽  
Author(s):  
Inmaculada Talaverano ◽  
Esperanza Valdés ◽  
Daniel Moreno ◽  
Esther Gamero ◽  
Luis Mancha ◽  
...  

2018 ◽  
Vol 59 (6) ◽  
pp. 815-826 ◽  
Author(s):  
Víctor Beyá-Marshall ◽  
Julio Herrera ◽  
Thomas Fichet ◽  
Eduardo R. Trentacoste ◽  
Cristián Kremer


2019 ◽  
Vol 16 (6) ◽  
pp. 1187-1209 ◽  
Author(s):  
Teamrat A. Ghezzehei ◽  
Benjamin Sulman ◽  
Chelsea L. Arnold ◽  
Nathaniel A. Bogie ◽  
Asmeret Asefaw Berhe

Abstract. Soil water status is one of the most important environmental factors that control microbial activity and rate of soil organic matter (SOM) decomposition. Its effect can be partitioned into effect of water energy status (water potential) on cellular activity, effect of water volume on cellular motility, and aqueous diffusion of substrate and nutrients, as well as the effect of air content and gas-diffusion pathways on concentration of dissolved oxygen. However, moisture functions widely used in SOM decomposition models are often based on empirical functions rather than robust physical foundations that account for these disparate impacts of soil water. The contributions of soil water content and water potential vary from soil to soil according to the soil water characteristic (SWC), which in turn is strongly dependent on soil texture and structure. The overall goal of this study is to introduce a physically based modeling framework of aerobic microbial respiration that incorporates the role of SWC under arbitrary soil moisture status. The model was tested by comparing it with published datasets of SOM decomposition under laboratory conditions.



1998 ◽  
Vol 103 (2-3) ◽  
pp. 295-300 ◽  
Author(s):  
E.L.B Novelli ◽  
R.T Hernandes ◽  
J.L.V.B Novelli Filho ◽  
L.L Barbosa


1994 ◽  
Vol 24 (1) ◽  
pp. 165-175 ◽  
Author(s):  
Yahia Abdel-Jawad ◽  
Muhammad Al-Qudah


1973 ◽  
Vol 10 (3) ◽  
pp. 403-407 ◽  
Author(s):  
Stephen Lakatos ◽  
Donald S. Miller

Discordant 'fission-track ages' on mica may be caused by (a) non-uniform uranium distribution, (b) addition or loss of uranium during the existence of the mineral, (c) thermal annealing of tracks, (d) inefficient etching of fossil tracks as compared to induced tracks in the mica, and (e) the effect of water pressure on track stability. The result of the combined effect of these factors causing discordant 'fission-track ages' on mica is at present unpredictable. Therefore, in the case of mica, interpretation of such ages is suspect.



1976 ◽  
Vol 16 (79) ◽  
pp. 272 ◽  
Author(s):  
D Pasternak ◽  
GL Wilson

The effect of water deficits on the relative photosynthetic rates in heads and leaves of sorghum was measured. When water was withheld, photosynthesis virtually ceased in the leaves but continued in the heads at the same rate. The photosynthetic activity of heads increased from about 12 per cent of the total in a well watered plant to about 88 per cent for a plant at high moisture deficit. Relative transpiration of heads also increased as water status declined. In watered plants, loss from heads was, like photosynthesis, about 12 per cent of the total but increased with water shortage to about 35 per cent.





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