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Patterns of water potential among forest types of the central Himalaya
Water potential (ψ) of soil and trees was measured in 16 forests from 450 to 2310 m elevation in the Kumaun Himalaya, during a two-year period. Predawn ψ, averaged across all species at a site was high (i.e. not stressful) at low elevations and variable at higher elevations. The incidence of low ψ a...
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Published in: | Current science (Bangalore) 2001-03, Vol.80 (6), p.774-779 |
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creator | Zobel, Donald B. Garkoti, Satish C. Singh, Surendra P. Tewari, Ashish Negi, C. M. S. |
description | Water potential (ψ) of soil and trees was measured in 16 forests from 450 to 2310 m elevation in the Kumaun Himalaya, during a two-year period. Predawn ψ, averaged across all species at a site was high (i.e. not stressful) at low elevations and variable at higher elevations. The incidence of low ψ at high elevations was opposite the usual pattern elsewhere. Midday ψ varied similarly. Patterns of plant and soil ψ differed. ψ values, especially in summer and winter, were severe enough to affect tree growth adversely. |
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M. S.</creatorcontrib><title>Patterns of water potential among forest types of the central Himalaya</title><title>Current science (Bangalore)</title><description>Water potential (ψ) of soil and trees was measured in 16 forests from 450 to 2310 m elevation in the Kumaun Himalaya, during a two-year period. Predawn ψ, averaged across all species at a site was high (i.e. not stressful) at low elevations and variable at higher elevations. The incidence of low ψ at high elevations was opposite the usual pattern elsewhere. Midday ψ varied similarly. Patterns of plant and soil ψ differed. ψ values, especially in summer and winter, were severe enough to affect tree growth adversely.</description><subject>Asia, Himalaya Mts</subject><subject>Coniferous forests</subject><subject>Forest soils</subject><subject>Forest stands</subject><subject>Plants</subject><subject>Rainy seasons</subject><subject>RESEARCH COMMUNICATIONS</subject><subject>Seasons</subject><subject>Soil water</subject><subject>Summer</subject><subject>Trees</subject><subject>Winter</subject><issn>0011-3891</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNotzs1KxDAUBeAsFBxHH0HIyl3h5qdpspTBcYSBcaHrctsm2tI2NckgfXuD4-pcOB-Xc0U2AIwVQht2Q25jHAC44GA2ZP-GKdkwR-od_cF80sUnO6ceR4qTnz-p88HGRNO62D-VvixtswhZHPoJR1zxjlw7HKO9_88t-dg_v-8OxfH08rp7OhYDB5WKDpzTUkkuWNOBQa51BayERlbcSHCdRaW5FSpXsmHalaVC26nWdbxtqkZsyePl7xL89znPqqc-tnYccbb-HGtWaWNMKTJ8uMAhJh_qJeShYa25ZFAqJcUvnKhR0Q</recordid><startdate>20010325</startdate><enddate>20010325</enddate><creator>Zobel, Donald B.</creator><creator>Garkoti, Satish C.</creator><creator>Singh, Surendra P.</creator><creator>Tewari, Ashish</creator><creator>Negi, C. 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Predawn ψ, averaged across all species at a site was high (i.e. not stressful) at low elevations and variable at higher elevations. The incidence of low ψ at high elevations was opposite the usual pattern elsewhere. Midday ψ varied similarly. Patterns of plant and soil ψ differed. ψ values, especially in summer and winter, were severe enough to affect tree growth adversely.</abstract><pub>Current Science Association</pub><tpages>6</tpages></addata></record> |
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language | eng |
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source | JSTOR Archival Journals and Primary Sources Collection |
subjects | Asia, Himalaya Mts Coniferous forests Forest soils Forest stands Plants Rainy seasons RESEARCH COMMUNICATIONS Seasons Soil water Summer Trees Winter |
title | Patterns of water potential among forest types of the central Himalaya |
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