Carbon fluxes, storage and harvest removals through 60 years of stand development in red pine plantations and mixed hardwood stands in Northern Michigan, USA

被引:25
作者
Gahagan, Adam [1 ]
Giardina, Christian P. [2 ]
King, John S. [3 ]
Binkley, Dan [4 ]
Pregitzer, Kurt S. [5 ]
Burton, Andrew J. [1 ]
机构
[1] Michigan Technol Univ, Sch Forest Resources & Environm Sci, Ecosyst Sci Ctr, Houghton, MI 49931 USA
[2] US Forest Serv, Inst Pacific Isl Forestry, USDA, Pacific Southwest Res Stn, Hilo, HI 96720 USA
[3] N Carolina State Univ, Dept Forestry & Environm Resources, Raleigh, NC 27695 USA
[4] Colorado State Univ, Dept Forest Rangeland & Watershed Stewardship, Ft Collins, CO 80523 USA
[5] Univ Idaho, Coll Nat Resources, Moscow, ID 83844 USA
关键词
Ecosystem carbon; Litterfall; Belowground; Productivity; Total belowground carbon flux; SOIL ORGANIC-CARBON; UPLAND FOREST ECOSYSTEMS; NET PRIMARY PRODUCTION; BELOW-GROUND BIOMASS; COARSE WOODY DEBRIS; SUGAR MAPLE FORESTS; SPATIAL VARIABILITY; NITROGEN DYNAMICS; CENTRAL WISCONSIN; ROOT RESPIRATION;
D O I
10.1016/j.foreco.2014.10.037
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The storage and flow of carbon (C) into and out of forests can differ under the influence of dominant tree species because of species-based variation in C production, decomposition, retention, and harvest-based export. Following abandonment of agricultural activities in the first half of the 20th century, many landscapes of the Great Lakes region (USA) were planted to red pine (Pinus resinosa) or naturally regenerated to northern hardwood species including sugar maple (Acer saccharum), red oak (Quercus rubra) and red maple (Acer rubrum). We located eight pairs of adjacent, similarly aged (similar to 60 yr) stands of planted red pine and naturally regenerated hardwood forests on previous agricultural fields. We found that the hardwood forests stored more C than pine stands (255 vs. 201 Mg C ha(-1)), with both storing substantially more than an adjacent area maintained as pasture (107 Mg C ha(-1)). The greater accumulation of C in the hardwood stands occurred mostly in living biomass. No significant differences for soil C (to 1 m depth) were found between forest types, despite significantly higher belowground inputs and above-ground litterfall in hardwood stands. Notably, both forest types had about 18% more soil C than the pasture, with O horizon C accounting for about one-third of the increase under trees. Forest type had no significant effect on estimated amount of exported C despite fairly large differences in projected end uses (solid wood products, land-fills, bioenergy). Using adjacent pasture as our baseline condition, we combined estimated on-site accumulation rates with estimates of exported C, and found that average total C sequestration rates were higher for hardwood (2.9 Mg C ha(-1) yr(-1)) than red pine plots (2.3 Mg C ha(-1) yr(-1)). The modeled potential contribution of exported C to these sequestration rate estimates did not differ between species, but the fate of modeled post-harvest off-site C may exert a large influence on sequestration rate estimates depending on actual displacement actions, including product longevity. These results show that tree species selection has the potential to impact C sequestration rates but effects vary by ecosystem component and could not be predicted from previous species effects studies. (C) 2014 Published by Elsevier B.V.
引用
收藏
页码:88 / 97
页数:10
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