The inhibiting effect of nitrate fertilisation on methane uptake of a temperate forest soil is influenced by labile carbon

被引:41
|
作者
Fender, Ann-Catrin [1 ]
Pfeiffer, Birgit [2 ]
Gansert, Dirk [1 ]
Leuschner, Christoph [1 ]
Daniel, Rolf [2 ]
Jungkunst, Hermann F. [2 ]
机构
[1] Univ Gottingen, D-37073 Gottingen, Germany
[2] Univ Gottingen, D-37077 Gottingen, Germany
关键词
CH4; uptake; NO3-; Glucose; Soil moisture; Interaction of C and N cycles; N deposition; METHYLOSINUS-TRICHOSPORIUM OB3B; ANAEROBICALLY DIGESTED CATTLE; ATMOSPHERIC METHANE; NITROGEN DEPOSITION; REACTIVE NITROGEN; CH4; OXIDATION; SULFUR DEPOSITION; CONIFEROUS FOREST; SPRUCE FOREST; N2O EMISSIONS;
D O I
10.1007/s00374-011-0660-3
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Upland soils are the most important terrestrial sink for the greenhouse gas CH4. The oxidation of CH4 is highly influenced by reactive N which is increasingly added to many ecosystems by atmospheric deposition and thereby also alters the labile C pool in the soils. The interacting effects of soil N availability and the labile C pool on CH4 oxidation are not well understood. We conducted a laboratory experiment with soil columns consisting of homogenised topsoil material from a temperate broad-leaved forest to study the net CH4 flux under the combined or isolated addition of NO (3) (-) and glucose as a labile C source. Addition of NO (3) (-) and glucose reduced the net CH4 uptake of the soil by 86% and 83%, respectively. The combined addition of both agents led to a nearly complete inhibition of CH4 uptake (reduction by 99.4%). Our study demonstrates a close link between the availability of C and N and the rate of CH4 oxidation in temperate forest soils. Continued deposition of NO (3) (-) has the potential to reduce the sink strength of temperate forest soils for CH4.
引用
收藏
页码:621 / 631
页数:11
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