Calcium and phosphorus interact to reduce mid-growing season net nitrogen mineralization potential in organic horizons in a northern hardwood forest

被引:21
作者
Minick, Kevan J. [1 ]
Fisk, Melany C. [1 ]
Groffman, Peter M. [2 ]
机构
[1] Miami Univ, Dept Zool, Oxford, OH 45056 USA
[2] Cary Inst Ecosyst Studies, Millbrook, NY 12545 USA
基金
美国国家科学基金会;
关键词
Acid deposition; Calcium; Gross nitrogen transformations; Microbial activity; Nutrient limitation; Phosphorus; Soil acidification; SUGAR MAPLE; MICROBIAL BIOMASS; ACID SOILS; ADIRONDACK MOUNTAINS; N MINERALIZATION; MATTER DYNAMICS; ACER-SACCHARUM; NITRIFICATION; CARBON; RATES;
D O I
10.1016/j.soilbio.2010.10.009
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Acid deposition can deplete soil calcium (Ca) and be detrimental to the health of some forests. We examined effects of soil Ca and phosphorus (P) availability on microbial activity and nitrogen (N) transformations in a plot-scale nutrient addition experiment at the Hubbard Brook Experimental Forest in New Hampshire, USA. We tested the hypotheses that (1) microbial activity and N transformations respond to large but not small changes in soil Ca, (2) soil Ca availability influences net N mineralization via the immobilization of N, rather than via changes in microbial activity, and (3) the response to Ca is constrained by P availability. Seasonality was a primary influence on the microbial response to treatments; N cycling processes varied from May to October and treatment effects were only detectable in the mid-growing season, in July. Neither microbial activity (C mineralization) nor gross N mineralization responded to Ca or to P. in either horizon. In the Oa horizon in July net N mineralization was reduced by high Ca and by Ca + P, and gross nitrification was increased by P addition. In the Oe horizon in July net N mineralization was reduced by Ca + P. These results partially supported our hypotheses, suggesting that soil Ca depletion has the potential to increase mid-growing season N availability via subtle changes in N immobilization, and that this effect is sensitive to soil P chemistry. The horizon-specific nature of the responses that we detected suggests that the proportions of Oe and Oa horizons comprising the surface organic layer will influence the relative importance of these processes at the ecosystem scale. Our results highlight the need for further attention to seasonal changes in controls of microbial mineralization/immobilization processes, to functional differences between organic horizons, and to interactions between Ca and Pin soils, in order to learn the specific mechanisms underlying the influence of Ca status on nutrient recycling in these northern hardwood ecosystems. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:271 / 279
页数:9
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