2016
DOI: 10.4236/ojf.2016.65025
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Disturbance Legacy on Soil Carbon Stocks and Stability within a Coastal Temperate Forest of Southwestern British Columbia, Canada

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Cited by 5 publications
(4 citation statements)
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“…Our finding that mineral soil C storage at 15-55 cm could be three times greater than C stored at 0-15 cm confirms the need to measure mineral soil C below 15 cm when calculating total ecosystem C, as recommended by Grand and Lavkulich (2011). In Pacific Northwest coastal forests, at least 50% of soil C storage is below 20 cm depth (Homann et al, 2005;Grand and Lavkulich, 2011;Defrenne et al, 2016) and Batjes (1996) reported an approximately 60% increase in the global soil organic C budget estimate if a second meter of soil is included in the calculation.…”
Section: Relationship Between Mineral Soil Carbon Stocks Depth and Climatesupporting
confidence: 66%
“…Our finding that mineral soil C storage at 15-55 cm could be three times greater than C stored at 0-15 cm confirms the need to measure mineral soil C below 15 cm when calculating total ecosystem C, as recommended by Grand and Lavkulich (2011). In Pacific Northwest coastal forests, at least 50% of soil C storage is below 20 cm depth (Homann et al, 2005;Grand and Lavkulich, 2011;Defrenne et al, 2016) and Batjes (1996) reported an approximately 60% increase in the global soil organic C budget estimate if a second meter of soil is included in the calculation.…”
Section: Relationship Between Mineral Soil Carbon Stocks Depth and Climatesupporting
confidence: 66%
“…The role of old age in a forest is also a rich field of research today. [16] For these reasons, the growth patterns in table 1 represent averages based on close reading of the USDA Silvics Manuals. [18] Therefore, on average, 1ft 2 of mass timber avoids 18 lbs CO2e of embodied carbon compared to concrete.…”
Section: Species Growth Patternsmentioning
confidence: 99%
“…The infrequency of disturbances (0.03%–0.84% area disturbed per year, 2000–2012; Buma et al 2017 ) combined with the longevity of many dominant tree species (often more than 500 years; Waring and Franklin 1979 ) means that, at broad temporal and spatial scales, materials export from forests to streams generally depends on climatically mediated changes in the hydrologic cycle itself. Increasing disturbance frequency may, however, have a negative effect on soil C stocks and stability because of disruption of the soil profile, alteration of infiltration and drainage, and changes in species composition (Defrenne et al 2016 ). Summer drought is driving increases in fire prevalence and extent in portions of the NPCTR, where this disturbance was historically infrequent (Reilly et al 2017 ) and increases in fire severity in areas in which fire was already important historically (Schoennagel et al 2017 ).…”
Section: Terrestrial Production and Delivery Of Materials To Surface Watersmentioning
confidence: 99%