Sustained effects of atmospheric [CO2] and nitrogen availability on forest soil CO2 efflux

被引:22
|
作者
Oishi, A. Christopher [1 ,2 ]
Palmroth, Sari [1 ,3 ]
Johnsen, Kurt H. [4 ]
Mccarthy, Heather R. [5 ]
Oren, Ram [1 ,3 ,6 ]
机构
[1] Duke Univ, Nicholas Sch Environm, Div Environm Sci & Policy, Durham, NC 27708 USA
[2] US Forest Serv, Coweeta Hyrdol Lab, Southern Res Stn, USDA, Otto, NC 28763 USA
[3] Swedish Univ Agr Sci SLU, Dept Forest Ecol & Management, SE-90183 Umea, Sweden
[4] US Forest Serv, Southern Res Stn, USDA, Res Triangle Pk, NC 27709 USA
[5] Univ Oklahoma, Dept Microbiol & Plant Biol, Norman, OK 73019 USA
[6] Duke Univ, Pratt Sch Engn, Dept Civil & Environm Engn, Durham, NC 27708 USA
基金
美国国家科学基金会;
关键词
automated soil respiration measurements; FACE; nitrogen fertilization; Pinus taeda; primary productivity; soil water content; FINE-ROOT PRODUCTION; LOBLOLLY-PINE FOREST; CANOPY LEAF-AREA; LONG-TERM GROWTH; ELEVATED CO2; CARBON ALLOCATION; TEMPERATE FOREST; DECIDUOUS FOREST; RESPIRATION; DYNAMICS;
D O I
10.1111/gcb.12414
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Soil CO2 efflux (F-soil) is the largest source of carbon from forests and reflects primary productivity as well as how carbon is allocated within forest ecosystems. Through early stages of stand development, both elevated [CO2] and availability of soil nitrogen (N; sum of mineralization, deposition, and fixation) have been shown to increase gross primary productivity, but the long-term effects of these factors on F-soil are less clear. Expanding on previous studies at the Duke Free-Air CO2 Enrichment (FACE) site, we quantified the effects of elevated [CO2] and N fertilization on F-soil using daily measurements from automated chambers over 10years. Consistent with previous results, compared to ambient unfertilized plots, annual F-soil increased under elevated [CO2] (ca. 17%) and decreased with N (ca. 21%). N fertilization under elevated [CO2] reduced F-soil to values similar to untreated plots. Over the study period, base respiration rates increased with leaf productivity, but declined after productivity saturated. Despite treatment-induced differences in aboveground biomass, soil temperature and water content were similar among treatments. Interannually, low soil water content decreased annual F-soil from potential values - estimated based on temperature alone assuming nonlimiting soil water content - by ca. 0.7% per 1.0% reduction in relative extractable water. This effect was only slightly ameliorated by elevated [CO2]. Variability in soil N availability among plots accounted for the spatial variability in F-soil, showing a decrease of ca. 114gCm(-2)yr(-1) per 1gm(-2) increase in soil N availability, with consistently higher F-soil in elevated [CO2] plots ca. 127gC per 100ppm [CO2] over the +200ppm enrichment. Altogether, reflecting increased belowground carbon partitioning in response to greater plant nutritional needs, the effects of elevated [CO2] and N fertilization on F-soil in this stand are sustained beyond the early stages of stand development and through stabilization of annual foliage production.
引用
收藏
页码:1146 / 1160
页数:15
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