119-3 The Effect of Different Forest Management Approaches on the C Stored in the Forest Floor and Soil of Loblolly Pine Plantations.

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range, and Wildland Soils General Session I Oral

Monday, November 7, 2016: 2:15 PM
Phoenix Convention Center North, Room 132 A

Jason G. Vogel1, Allan Bacon2, Rosvel Bracho3, Eric Jokela3, Sabine Grunwald4, Thomas R. Fox5, Marshal Laviner6, C. Wade Ross7, Michael Kane8, Daniel Markewitz9, Harold Burkhart10, Joshua Cucinella11, Tim Martin3 and Madison Akers12, (1)Department of Ecosystem Science and Management, Texas A&M University, College Station, TX
(2)PO Box 110290, University of Florida, Gainesville, FL
(3)School of Forest Resources and Conservation, University of Florida, Gainesville, FL
(4)Soil and Water Sciences Department, University of Florida, Gainesville, FL
(5)228 Cheatham Hall, Virginia Tech, Blacksburg, VA
(6)The Department of Forest Resources and Environmental Conservation, Virginia Tech, Blacksburg, VA
(7)Soil and Water Science Department, University of Florida, Gainesville, FL
(8)Warnell School of Forestry and Natural Resources, The University of Georgia, Athens, GA
(9)Forestry and Natural Resources, University of Georgia - Athens, Athens, GA
(10)Virginia Tech, Blacksburg, VA
(11)School of Forest Resources and Conservation, Gainesville, FL
(12)Warnell School of Forestry and Natural Resources, University of Georgia, Athens, GA
Abstract:
Extending from Virginia to east Texas in the southeastern United States, managed pine plantations are an important component of the region’s carbon cycle. An objective of the Pine Integrated Network: Education, Mitigation, and Adaptation project (PINEMAP) is to improve estimates of how ecosystem carbon pools respond to the management strategies used to increase the growth of loblolly pine plantations.  Experimental studies (108 total) that had historically been used to understand forest productivity and stand dynamics by university-forest industry cooperatives were measured for the carbon stored in the trees, coarse-wood, forest floor, understory and soils to 1-meter (0-10 cm, 10-20 cm, 20-50 cm, and 50-100 cm).  The age of the studied plantations ranged from 4-26 years at the time of sampling, with 26 years very near the period when these plantations are commonly harvested. The study sites encapsulated a wide regional range in precipitation (1080 mm -1780 mm) and potential evapotranspiration (716 mm – 1200 mm). The most prevalent three soil orders measured were Ultisols (62%), Alfisols (19%), and Spodosols (10%) with Entisols, Inceptisols and 1 Histosol making up the remainder (9%).

Across all study sites, 455 experimental plots were measured. The plots had as a treatment either fertilization, competition control, and stand density control (thinning), including every possible combination of treatments (including ‘no treatment’).  Across all treatment combinations an increase in forest biomass correlated with an increase forest floor C but there was no overall correlation between tree biomass and soil C change. Paired treatment combinations were examined, and for soil and forest floor C pools a consistent treatment effect was where thinning caused a pool of C decrease relative to an unthinned treatment.  These results suggest maintaining higher tree densities would result in greater forest floor and soil C pools in pine plantations.

See more from this Division: SSSA Division: Forest, Range and Wildland Soils
See more from this Session: Forest, Range, and Wildland Soils General Session I Oral