Dynamic aspects of soil water availability for isohydric plants: Focus on root hydraulic resistances. Issue 11 (18th November 2014)

• Record Type: Journal Article
• Authors: Couvreur, V.; Vanderborght, J.; Draye, X.; Javaux, M.
• Is Part Of: Water resources research. Volume 50:Issue 11(2014:Nov.)
• Page Start: 8891
• Page End: 8906
• Publication Date: 2014-11-18
• Subjects: Hydrology -- Periodicals; 333.91
• DOI: 10.1002/2014WR015608
• Languages: English
• ISSNs: 0043-1397

Abstract

<abstract abstract-type="main"> <title>Abstract</title> <p>Soil water availability for plant transpiration is a key concept in agronomy. The objective of this study is to revisit this concept and discuss how it may be affected by processes locally influencing root hydraulic properties. A physical limitation to soil water availability in terms of maximal flow rate available to plant leaves ( <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4fj9" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0001" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mrow><mml:mtext>avail</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula>) is defined. It is expressed for isohydric plants, in terms of plant‐centered variables and properties (the equivalent soil water potential sensed by the plant, <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4ffn" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0002" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>ψ</mml:mi><mml:mrow><mml:mi mathvariant="normal">s</mml:mi><mml:mo> </mml:mo><mml:mo> </mml:mo><mml:mtext>eq</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula>; the root system equivalent conductance, <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4fd3" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0003" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>K</mml:mi><mml:mrow><mml:mtext>rs</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula>; and a threshold leaf water potential, <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4ftq" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0004" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>ψ</mml:mi><mml:mrow><mml:mtext>leaf</mml:mtext><mml:mo> </mml:mo><mml:mtext>lim</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula>). The resulting limitation to plant transpiration is compared to commonly used empirical stress functions. Similarities suggest that the slope of empirical functions might correspond to the ratio of <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4frm" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0005" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>K</mml:mi><mml:mrow><mml:mtext>rs</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula> to the plant potential transpiration rate. The sensitivity of <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4fph" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0006" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mrow><mml:mtext>avail</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula> to local changes of root hydraulic conductances in response to soil matric potential is investigated using model simulations. A decrease of radial conductances when the soil dries induces earlier water stress, but allows maintaining higher night plant water potentials and higher <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4fnz" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0007" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mrow><mml:mtext>avail</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula> during the last week of a simulated 1 month drought. In opposition, an increase of radial conductances during soil drying provokes an increase of hydraulic redistribution and <inline-formula><alternatives><inline-graphic mimetype="image" xlink:href="ark:/27927/pgh2wqg4d7t" xlink:type="simple" xmlns:xlink="http://www.w3.org/1999/xlink" /><mml:math display="inline" altimg="urn:x-wiley:00431397:media:wrcr21212:wrcr21212-math-0008" overflow="scroll" xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mrow><mml:mtext>avail</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></alternatives></inline-formula> at short term. This study offers a first insight on the effect of dynamic local root hydraulic properties on soil water availability. By better understanding complex interactions between hydraulic processes involved in soil‐plant hydrodynamics, better prospects on how root hydraulic traits mitigate plant water stress might be achieved.</p> </abstract>