Decomposing litter as a sink for 15N-enriched additions to an oak forest and a red pine plantation

被引:85
作者
Micks, P
Downs, MR
Magill, AH
Nadelhoffer, KJ
Aber, JD
机构
[1] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
[2] LaGrange St, W Roxbury, MA 02132 USA
[3] Univ New Hampshire, Complex Syst Res Ctr, Durham, NH 03824 USA
[4] Univ Michigan, Dept Ecol & Evolutionary Biol, Ann Arbor, MI 48109 USA
基金
美国国家科学基金会;
关键词
litter decomposition; ammonium and nitrate additions; N-15; tracers; nitrogen deposition; forest nitrogen storage;
D O I
10.1016/j.foreco.2004.03.013
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
The importance of surface litter as a sink for atmospheric N deposition on forests was investigated using N-15 tracers to quantify the effects of N input rate and litter age on retention of N inputs by forest litter. The study was conducted in plots receiving ambient (0.8 a N m(-2) per year) and chronically elevated N inputs (ambient + 5 g NH4NO3-N m(-2) per year) in both a hardwood forest and a red pine plantation. Plots (30 m x 30 m) were part of the Chronic Nitrogen Amendment Study at the Harvard Forest, Massachusetts, USA. To allow estimates of N sink strength in litter cohorts of two different ages, litterbags containing oak leaves, maple leaves, pine needles, or maple wood chips were placed in the plots in years 1 and 3 of fertilizer additions. Uptake of N inputs into decomposing litter was estimated using N-15 tracers applied as (NH4)-N-15 or (NO3)-N-15 during years 4 and 5 of fertilizer additions. Thus N-15 additions occurred to litters in their fourth and fifth years of decay (set out in year 1 of N additions) and to litters in their second and third years of decay (set out in year 3 of N additions). The effect of N input level on mass loss and N dynamics varied among litter types and appeared to increase with litter age. Fertilization decreased mass loss and loss of initial N content in maple and oak leaf litters, but it enhanced mass loss in wood and had little effect on pine needles. Decomposing litter cohorts in both forests retained significant proportions of N inputs at both ambient (20% in hardwood. 9% in pine) and elevated levels (7% in hardwood, 6% in pine) over the 2 years of tracer additions. Tracer assimilation into the 2-year-old litter cohort decreased under elevated N inputs, NO3- assimilation decreased relative to NH4+ and assimilation of both forms was lower in 4-year-old material on a per unit litter mass basis. Ecosystem-scale retention of N inputs by the 2 + 4-year-old litter cohorts in both forests increased with N input level, from 0.32 and 0.15 g N m(-2) over 2 years (ambient hardwood and pine plots) to 0.86 and 0.70 g N m(-2) over 2 years (fertilized hardwood and pine plots). Although N sink strength of litter pools increased more strongly in the pine forest in response to elevated N inputs, the hardwood forest retained more N under both input levels, suggesting that it may be a larger sink for atmospheric N deposition than the pine forest. Recently formed litter pools assimilate more NO3 than NH4+. under ambient N deposition, but may lose capacity to assimilate NO3- relative to NH4+ under potential future increases in N deposition. (C) 2004 Elsevier B.V. All rights reserved.
引用
收藏
页码:71 / 87
页数:17
相关论文
共 44 条
[1]   Nitrogen saturation in temperate forest ecosystems - Hypotheses revisited [J].
Aber, J ;
McDowell, W ;
Nadelhoffer, K ;
Magill, A ;
Berntson, G ;
Kamakea, M ;
McNulty, S ;
Currie, W ;
Rustad, L ;
Fernandez, I .
BIOSCIENCE, 1998, 48 (11) :921-934
[2]   PREDICTING LONG-TERM PATTERNS OF MASS-LOSS, NITROGEN DYNAMICS, AND SOIL ORGANIC-MATTER FORMATION FROM INITIAL FINE LITTER CHEMISTRY IN TEMPERATE FOREST ECOSYSTEMS [J].
ABER, JD ;
MELILLO, JM ;
MCCLAUGHERTY, CA .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1990, 68 (10) :2201-2208
[3]   NITROGEN IMMOBILIZATION IN DECAYING HARDWOOD LEAF LITTER AS A FUNCTION OF INITIAL NITROGEN AND LIGNIN CONTENT [J].
ABER, JD ;
MELILLO, JM .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1982, 60 (11) :2263-2269
[4]  
BAATH E, 1981, ZBL BAKT MIK HYG I C, V2, P90
[5]   DYNAMICS OF NITROGEN (N-15) IN DECOMPOSING SCOTS PINE (PINUS-SYLVESTRIS) NEEDLE LITTER - LONG-TERM DECOMPOSITION IN A SCOTS PINE FOREST .6. [J].
BERG, B .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1988, 66 (08) :1539-1546
[6]   NITROGEN AND PHOSPHORUS RELEASE FROM DECOMPOSING LITTER IN RELATION TO THE DISAPPEARANCE OF LIGNIN [J].
BERG, B ;
MCCLAUGHERTY, C .
CANADIAN JOURNAL OF BOTANY-REVUE CANADIENNE DE BOTANIQUE, 1989, 67 (04) :1148-1156
[7]   Nutrient Release from Litter and Humus in Coniferous Forest Soils-a Mini Review [J].
Berg, Bjorn .
SCANDINAVIAN JOURNAL OF FOREST RESEARCH, 1986, 1 (1-4) :359-369
[8]   Long-term decomposition of successive organic strata in a nitrogen saturated Scots pine forest soil [J].
Berg, MP ;
Kniese, JP ;
Zoomer, R ;
Verhoef, HA .
FOREST ECOLOGY AND MANAGEMENT, 1998, 107 (1-3) :159-172
[9]   Interactive effects of pH and substrate quality on the fungal-to-bacterial ratio and QCO2 of microbial communities in forest soils [J].
Blagodatskaya, EV ;
Anderson, TH .
SOIL BIOLOGY & BIOCHEMISTRY, 1998, 30 (10-11) :1269-1274
[10]   ANNUAL NITROUS-OXIDE FLUXES FROM TEMPERATE FOREST SOILS IN THE NORTHEASTERN UNITED-STATES [J].
BOWDEN, RD ;
STEUDLER, PA ;
MELILLO, JM ;
ABER, JD .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D9) :13997-14005