Long- and short-term precipitation effects on soil CO2 efflux and total belowground carbon allocation

被引:24
作者
Ford, Chelcy R. [1 ]
McGee, Jason [2 ]
Scandellari, Francesca [2 ,3 ]
Hobbie, Erik A. [3 ]
Mitchell, Robert J. [2 ]
机构
[1] USDA FS SRS Coweeta Hydrol Lab, Otto, NC 28763 USA
[2] Joseph W Jones Ecol Res Ctr, Newton, GA 39870 USA
[3] Univ New Hampshire, Durham, NH 03824 USA
关键词
Carbon allocation; Climate change; Longleaf pine; Irrigation; Root demography; Soil respiration; PONDEROSA PINE PLANTATION; LOBLOLLY-PINE; ROOT-GROWTH; FINE-ROOT; RESPIRATION; WATER; FOREST; TEMPERATURE; DYNAMICS; NUTRIENT;
D O I
10.1016/j.agrformet.2011.12.008
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Soil CO2 efflux (E-soil). the main pathway of C movement from the biosphere to the atmosphere, is critical to the terrestrial C cycle but how precipitation and soil moisture influence E-soil remains poorly understood. Here, we irrigated a longleaf pine wiregrass savanna for six years; this increased soil moisture by 41.2%. We tested how an altered precipitation regime affected total belowground carbon allocation (TBCA), root growth, soil carbon, and E-soil. We used two methods to quantify E-soil: daytime biweekly manual measurements and automated continuous measurements for one year. we hypothesized that the low-frequency manual method would miss both short- and long-term (i.e., subdaily to annual, respectively) effects of soil moisture on E-soil while the high-frequency data from the automated method would allow the effects of soil moisture to be discerned. Root growth was significantly higher in irrigated plots, particularly at 0-20 cm depth. Irrigated annual E-soil was significantly greater than that of the control when estimated with the continuous measurements but not when estimated from biweekly measurements. The difference in annual E-soil estimates is likely due to (1) the delayed increase in E-soil following irrigation pulses of soil moisture (i.e., variation that the biweekly manual measurements missed) and (2) the diel timing of biweekly manual measurements (they were completed early to mid-day before peak efflux). With irrigation, estimates of TBCA increased almost two-fold with automated measurements but only 36% with intermittent measurements. Relative to controls, irrigated treatments stored almost 2 Mg C ha(-1) year(-1) more in soils and 0.26 Mg C ha(-1) year(-1) more in roots. High-frequency measurements of E-soil were essential to estimate total belowground carbon allocation. With irrigation, soil carbon pools were not at steady-state, so shifts in soil carbon storage must be considered in TBCA estimates. Published by Elsevier B.V.
引用
收藏
页码:54 / 64
页数:11
相关论文
共 71 条
[1]   Adjustments in hydraulic architecture of Pinus palustris maintain similar stomatal conductance in xeric and mesic habitats [J].
Addington, RN ;
Donovan, LA ;
Mitchell, RJ ;
Vose, JM ;
Pecot, SD ;
Jack, SB ;
Hacke, UG ;
Sperry, JS ;
Oren, R .
PLANT CELL AND ENVIRONMENT, 2006, 29 (04) :535-545
[2]  
Albaugh TJ, 1998, FOREST SCI, V44, P317
[3]  
[Anonymous], 1998, Environmental Soil Physics: Fundamentals, Applications, and Environmental Considerations
[4]   How switches and lags in biophysical regulators affect spatial-temporal variation of soil respiration in an oak-grass savanna [J].
Baldocchi, Dennis ;
Tang, Jianwu ;
Xu, Liukang .
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES, 2006, 111 (G2)
[5]   The relative controls of temperature, soil moisture, and plant functional group on soil CO2 efflux at diel, seasonal, and annual scales [J].
Barron-Gafford, Greg A. ;
Scott, Russell L. ;
Jenerette, G. Darrel ;
Huxman, Travis E. .
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES, 2011, 116
[6]  
Birch H. F., 1964, Plant and Soil, V20, P43, DOI 10.1007/BF01378096
[7]   Temperature-associated increases in the global soil respiration record [J].
Bond-Lamberty, Ben ;
Thomson, Allison .
NATURE, 2010, 464 (7288) :579-U132
[8]   Simulated chronic NO3- deposition reduces soil respiration in northern hardwood forests [J].
Burton, AJ ;
Pregitzer, KS ;
Crawford, JN ;
Zogg, GP ;
Zak, DR .
GLOBAL CHANGE BIOLOGY, 2004, 10 (07) :1080-1091
[9]  
Campbell Scientific Inc, 2002, INSTR MAN CS616 CS62, P48
[10]  
Carbone MS, 2008, NEW PHYTOL, V177, P295