Methane Emissions from a Grassland-Wetland Complex in the Southern Peruvian Andes

被引:5
|
作者
Jones, Sam P. [1 ,2 ]
Diem, Torsten [3 ]
Teh, Yit Arn [3 ]
Salinas, Norma [4 ]
Reay, Dave S. [1 ]
Meir, Patrick [1 ,5 ]
机构
[1] Univ Edinburgh, Sch Geosci, Edinburgh EH8 9XP, Midlothian, Scotland
[2] INRA, UMR 1391 ISPA, F-33140 Villenave Dornon, France
[3] Univ Aberdeen, Inst Biol & Environm Sci, Aberdeen AB24 3UU, Scotland
[4] Pontificia Univ Catolica Peru, Inst Ciencias Naturaleza Terr & Energias Renovabl, Lima 15088, Peru
[5] Australian Natl Univ, Res Sch Biol, Acton, ACT 2601, Australia
基金
澳大利亚研究理事会; 英国自然环境研究理事会;
关键词
soil; methanogenesis; methanotrophy; upland; peatland; puna; POOL DILUTION TECHNIQUE; MONTANE FOREST SOILS; NITROUS-OXIDE FLUXES; ATMOSPHERIC METHANE; SEASONAL VARIABILITY; CH4; PRODUCTION; FERRIC IRON; LAND-USE; CARBON; OXIDATION;
D O I
10.3390/soilsystems3010002
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Wet organic-rich mineral and peat soils in the tropical Andes represent a potentially significant, but little studied, source of methane to the atmosphere. Here we report the results of field and laboratory measurements of soil-atmosphere methane exchange and associated environmental variables from freely draining upland and inundation prone wetland soils in a humid puna ecosystem in the Southeastern Andes of Peru. Between seasons and across the landscape soil-atmosphere exchange varied between uptake and emission. Notable hotspots of methane emission, peaking during the wet season, were observed from both upland and wetland soils with particularly strong emissions from moss-accumulating topographic lows. This variability was best explained by the influence of oxygen concentration on methane production in superficial soil horizons.
引用
收藏
页码:1 / 21
页数:21
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