首页> 外文期刊>European Journal of Soil Biology >Priming effects of Aporrectodea caliginosa on young rhizodeposits and old soil organic matter following wheat straw addition
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Priming effects of Aporrectodea caliginosa on young rhizodeposits and old soil organic matter following wheat straw addition

机译:加麦草后白线孢菌对幼根茎和旧土壤有机质的引发作用

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摘要

Previous work has shown that endogeic earthworms cause different, i.e. apparent as well as true positive priming effects, presumably due to unknown interactions of substrate-colonising fungi and labile SOM, e.g. rhizodeposits. To explore these interactions, a soil that had previously been enriched with C-13- and N-15-labelled rhizodeposits of pea (Pisum sativum L) plants was used in an incubation experiment. The objective was to determine whether Aporrectodea caliginosa causes a priming effect on the decomposition of young rhizodeposits and old soil organic matter (SOM) following wheat straw addition. After 56 days of incubation at 12 degrees C, earthworm effects on autochthonous SOM-derived CO2 (+88%) were higher than on rhizodeposit-derived CO2 (+16%), indicating a stronger true positive priming effect on old SOM than on young rhizodeposits. Feeding of A. caliginosa significantly reduced microbial biomass C (-12%) and N (-30%) derived from rhizodeposits. In contrast, SOM-derived microbial biomass C and N remained unaffected, indicating a higher palatability of rhizodeposits. However, they were not catabolized to CO2, but preferentially anabolized, i.e. transferred to the biomass of microorganisms and earthworms. Not only straw but also A. caliginosa generally caused a shift in the microbial community towards saprotrophic fungi, as indicated by increased ergosterol contents and ergosterol to microbial biomass C ratios. A. caliginosa decreased delta N-15, total N, and N derived from rhizodeposits in the non-decomposed straw recovered as particulate organic matter, indicating the importance of rhizodeposits as an N source. (C) 2015 Elsevier Masson SAS. All rights reserved.
机译:先前的研究表明,内生earth引起不同的,即表观的和真正的正启动效应,大概是由于底物定殖真菌和不稳定的SOM(例如SOM)的相互作用未知。根状茎。为了探索这些相互作用,在培养实验中使用了以前富含豌豆(Pisum sativum L)植物的C-13和N-15标记的根状土壤的土壤。目的是确定加麦草后,Aporrectodea caliginosa是否引起对幼根茎沉积和旧土壤有机质(SOM)分解的引发作用。在12摄氏度下温育56天后,worm对自体SOM来源的CO2的影响(+ 88%)高于对根茎来源的CO2(+ 16%)的影响,表明对老SOM的真实阳性启动作用要强于对年轻SOM的作用。根状茎。 caliginosa的饲喂显着降低了来源于根茎菌的微生物生物量C(-12%)和N(-30%)。相反,源自SOM的微生物生物量C和N保持不受影响,表明根状茎的适口性更高。但是,它们没有被分解为二氧化碳,而是被优先合成代谢,即转移到微生物和earth的生物质中。如麦角固醇含量增加和麦角固醇与微生物生物质C的比率增加所表明的,不仅秸秆,而且caliginosa曲霉通常还引起微生物群落向腐生真菌的转移。 caliginosa A. caliginosa降低了未分解秸秆中作为根状有机物回收的根际沉积物的δN-15,总氮和氮,表明根际沉积物作为氮源的重要性。 (C)2015 Elsevier Masson SAS。版权所有。

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