Earthworm-induced N2O emissions in a sandy soil with surface-applied crop residues

被引:14
|
作者
Giannopoulos, Georgios [1 ]
van Groenigen, Jan Willem [1 ]
Pulleman, Mirjam M. [1 ]
机构
[1] Wageningen Univ, Dept Soil Qual, NL-6700 AA Wageningen, Netherlands
关键词
Earthworms; Endogeic; Epigeic; Nitrous oxide; N-15; Soil organic matter turnover; NITROUS-OXIDE EMISSIONS; NITRIFIER DENITRIFICATION; ORGANIC-MATTER; CARBON; AGGREGATION; DYNAMICS; BIOTA;
D O I
10.1016/j.pedobi.2011.09.005
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Earlier research with endogeic and epigeic earthworm species in loamy arable soil has shown that both earthworm groups can increase nitrous oxide (N2O) emissions, provided that crop residue placement matches the feeding strategy of the earthworm ecological group(s). However, it is not yet clear whether these effects also occur in sandy soils which typically contain less soil organic matter and have low soil aggregation levels. Here, we aimed to quantify N2O emissions as affected by endogeic and/or epigeic earthworm species, and to relate changes in N2O emissions to earthworm-induced changes in soil properties in a sandy soil. A 90 day mesocosm study was conducted with sandy soil and N-15-labeled radish (Raphanus sativus cv. Adagio L) residue applied on top. Treatments included: (i) no earthworm addition, (ii) addition of the endogeic species Aporrectodea caliginosa (Savigny), (iii) addition of the epigeic species Lumbricus rubellus (Hoffmeister), and (iv) both species combined. An additional treatment was included without earthworms and with residue manually incorporated into the soil. L rubellus significantly increased cumulative N2O emissions from 228 to 859 mu g N2O-N kg(-1) (F-1,F-12=83.12, P<0.001), whereas A. caliginosa did not affect N2O emissions. In contrast to earlier studies in loamy soil, no positive interaction between both species with regard to N2O emissions was found. This was probably related to high competition for organic resources in the relatively poor soil and a low potential for stable soil aggregate formation (and associated anaerobic microsites) by endogeic worms in sandy soil. N-15 isotope analysis revealed that the activity of L. rubellus significantly increased (F-1,F-12=6.20, P=0.028) the recovery of N-15 in the 250-8000 mu m size fraction, indicating incorporation of crop residues into the mineral soil. When residues were manually incorporated, N2O emissions were significantly (P<0.008) lower (509 mu g N2O-N kg(-1)) than when incorporated by L rubellus. The high N2O emissions in the presence of L rubellus, when compared to manual mixing, suggest a stimulation of microbial activity and/or changes in the microbial community composition. Insights on the earthworm effects on N2O emission from such soils are discussed. (C) 2011 Elsevier GmbH. All rights reserved.
引用
收藏
页码:S103 / S111
页数:9
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