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Earthworm-induced N _2O emissions in a sandy soil with surface-applied crop residues

机译:worm在表层残留农作物的沙质土壤中的N _2O排放

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Earlier research with endogeic and epigeic earthworm species in loamy arable soil has shown that both earthworm groups can increase nitrous oxide (N _2O) 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 N _2O emissions as affected by endogeic and/or epigeic earthworm species, and to relate changes in N _2O emissions to earthworm-induced changes in soil properties in a sandy soil. A 90 day mesocosm study was conducted with sandy soil and ~(15)N-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 N _2O emissions from 228 to 859μg N _2O-Nkg ~(-1) (F _(1,12)=83.12, P<0.001), whereas A. caliginosa did not affect N _2O emissions. In contrast to earlier studies in loamy soil, no positive interaction between both species with regard to N _2O 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. ~(15)N isotope analysis revealed that the activity of L. rubellus significantly increased (F _(1,12)=6.20, P=0.028) the recovery of ~(15)N in the 250-8000μm size fraction, indicating incorporation of crop residues into the mineral soil. When residues were manually incorporated, N _2O emissions were significantly (P<0.008) lower (509μg N _2O-Nkg ~(-1)) than when incorporated by L. rubellus. The high N _2O 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 N _2O emission from such soils are discussed.
机译:早先在壤土耕地中对内生和表皮earth物种进行的研究表明,只要作物残茬的放置与the生态群的摄食策略相匹配,both的两个组都可以增加一氧化二氮(N _2O)的排放。然而,尚不清楚这些影响是否也发生在通常含有较少土壤有机质和低土壤聚集水平的沙质土壤中。在这里,我们旨在量化受内生和/或表生epi物种影响的N _2O排放量,并将N _2O排放量的变化与earth引起的沙质土壤性质的变化联系起来。进行了90天的中观研究,将沙质土壤和〜(15)N标记的萝卜(Raphanus sativus cv。Adagio L.)残留物涂在顶部。处理方法包括:(i)不添加,,(ii)添加内生物种califorosa caliginosa(Savigny),(iii)添加流行物种Lumbricus rubellus(Hoffmeister),和(iv)将两个物种合并。包括没有without的其他处理,并且将残留物手动掺入土壤中。风疹杆菌将累积N _2O排放从228μgN _2O-Nkg〜(-1)显着增加(F _(1,12)= 83.12,P <0.001),而whereas游曲霉不影响N _2O的排放。与在壤土中的早期研究相反,在N _2O排放方面,没有发现两个物种之间存在正向相互作用。这可能与相对贫瘠的土壤中有机资源的激烈竞争以及沙质土壤中的内生蠕虫形成稳定的土壤团聚体(以及相关的厌氧性微场所)的可能性较低有关。 〜(15)N同位素分析表明,在250-8000μm粒径级分中,〜(15)N的回收率显着提高了风疹乳杆菌的活性(F _(1,12)= 6.20,P = 0.028)。作物残渣进入矿物土壤。手动掺入残渣时,N.O的排放量比风铃草所掺入的低得多(P <0.008)(509μgN _2O-Nkg〜(-1))。与人工混合相比,在风疹乳酸菌存在下高的N _2O排放量表明刺激了微生物活性和/或微生物群落组成的变化。讨论了worm对此类土壤中N _2O排放的影响的见解。

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