Seasonal shifts in depth-to-water uptake by young thinned and overstocked lodgepole pine (Pinus contorta) forests under drought conditions in the Okanagan Valley, British Columbia, Canada
Department of Earth, Environmental and Geographic Sciences, University of British Columbia (Okanagan Campus), Kelowna, British Columbia, V1V 1V7, Canada
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Cumulative views and downloads
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Total article views: 1,529 (including HTML, PDF, and XML)
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954
311
264
1,529
84
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74
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Supplement: 84
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EndNote: 74
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Total article views: 446 (including HTML, PDF, and XML)
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328
84
34
446
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Total: 446
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Cumulative views and downloads
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Total article views: 1,975 (including HTML, PDF, and XML)
Thereof 1,905 with geography defined
and 70 with unknown origin.
Total article views: 1,529 (including HTML, PDF, and XML)
Thereof 1,474 with geography defined
and 55 with unknown origin.
Total article views: 446 (including HTML, PDF, and XML)
Thereof 431 with geography defined
and 15 with unknown origin.
This study analyzes water-stable isotope composition by analyzing the impact of forest thinning on lodgepole pine depth-to-water uptake and water-use strategies. Lodgepole pine's primary source is spring snowmelt and shifts to rely on deeper soil water to maintain water uptake. There was no effect of decreased stand density on depth-to-water uptake. It will become more critical that we know how much water forests are using and which strategies trees use to sustain their water supply.
This study analyzes water-stable isotope composition by analyzing the impact of forest thinning...