Water influx characteristics and hydraulic conductivity for roots of Agave deserti Engelm (Record no. 51211)

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control field MX-MdCICY
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control field 20250625160203.0
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Transcribing agency CICY
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Classification number (OCLC) (R) ; Classification number, CALL (RLIN) (NR) B-17048
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fixed length control field 250602s9999 xx |||||s2 |||| ||und|d
245 10 - TITLE STATEMENT
Title Water influx characteristics and hydraulic conductivity for roots of Agave deserti Engelm
490 0# - SERIES STATEMENT
Volume/sequential designation Journal of Experimental Botany, 41(4), p.409-415, 1990
520 3# - SUMMARY, ETC.
Summary, etc. Various plant and environmental factors influence the hydraulic properties for roots, which were examined using negative hydrostatic pressures applied to the proximal ends of individual excised roots of a common succulent perennial from the Sonoran Desert, Agave deserti Engelm. The root hydraulic conductivity, Lp, increased substantially with temperature, the approximately 4-fold increase from 0.5°C to 40°C representing a Q10 of 1.45. Such variations in Lp with temperature must be taken into account when modelling water uptake, as soil temperatures in the root zone of such a shallow-rooted species vary substantially both daily and seasonally. At 20°C, Lp was 2.3 × 10?7 m s¯1MPa¯1for 3-week-old roots, decreasing to about half this value at 10 weeks and then becoming approximately halved again at 6 months. For a given root age, Lp for rain roots that are induced by watering as lateral branches on the established roots (which arise from the stem base)was about the same as Lp for established roots. Hence, the conventional belief that rain roots have a higher Lp than do established roots is more a reflection of root age, as the rain roots tend to be shed following drought and thus on average are much younger than are established roots. Unlike previous measurements on root respiration, lowering the gas-phase oxygen concentration from 21 percent to 0 percent or raising the carbon dioxide concentration from 0.1 percent to 2 percent had no detectable effect on Lp for rain roots and established roots. Lp for rain roots and established roots was decreased by an average of 11 percent and 35 percent by lowering the soil water potential from wet conditions (?soil=0 kPa)to ¯40 kPa and ¯80 kPa, respectively. Such decreases in Lp may reflect reduced water contact between soil particles and the root surface and should be taken into account when predicting water uptake by A. deserti.
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GAS PHASE
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element RAIN ROOTS
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element ROOT AGE
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element SOIL
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element TEMPERATURE
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element WATER POTENTIAL
700 12 - ADDED ENTRY--PERSONAL NAME
Personal name Nobel, P. S.
700 12 - ADDED ENTRY--PERSONAL NAME
Personal name Schulte, P. J.
700 12 - ADDED ENTRY--PERSONAL NAME
Personal name North, G. B.
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier <a href="https://drive.google.com/file/d/15KkMHEnaQeHvHYX8QC4JzfbH8B53CuZN/view?usp=drivesdk">https://drive.google.com/file/d/15KkMHEnaQeHvHYX8QC4JzfbH8B53CuZN/view?usp=drivesdk</a>
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