ВЛИЯНИЕ АЗОТА НА МИНЕРАЛИЗАЦИЮ И ГУМИФИКАЦИЮ ЛЕСНЫХ ОПАДОВ В МОДЕЛЬНОМ ЭКСПЕРИМЕНТЕ
Notice bibliographique
Résumé
RUSSIAN JOURNAL OF FOREST SCIENCE. 2017, No. 2, pp. 128-139 THE CONTRIBUTION OF NITROGEN TO MINERALIZATION AND HUMIFICATION OF FOREST LITTER IN SIMULATION STUDY A. A. Larionova 1 , A. K. Kvitkina 1 , S. S. Bykhovets 1 , V. O. Lopes-de-Gerenyu 1 , Y. G. Kolyagin 2 , V. V. Kaganov 3 1 Institute of Physicochemical and Biological Problems of Soil Sciences, Russian Academy of Sciences Institutskaya st., 2, Pushchino, Moscow Oblast, 142290, Russia E-mail: larionova_al@rambler.ru 2 Faculty of Chemistry, Lomonosov Moscow State University Leninskie gory, 1, bldg.3, Moscow, 119991, Russia 3 Center for Forest Ecology and Productivity of the Russian Academy of Sciences Profsoyuznaya st., 84/32, bldg. 14, Moscow, 117997, Russia Received 16 June 2016 We carried out long-term incubations to study the contribution of endogenous and exogenous nitrogen to decomposition of various fractions of forest litter, sampled in linden, pine and aspen mixed forest in Prioksko-Terrasny Nature Reserve. Based on C:N ratio signatures (including endogenous nitrogen) the following sequence was found: mortmass of cyanobacteria Nostoсcommunae (C:N ratio 9), deciduous litter (C:N ratio 32), pine needles litter (C:N ratio 66), pine bark litter (C:N ratio 84), coarse woody debris of linden (C:N ratio 206), coarse woody debris of pine (C:N ratio 510). To find the effect of exogenous nitrogen we applied NH 4 NO 3 to the litters until the prescribed C:N ratio in the range of 5 to 204 has been reached. Mineralization was assessed by CO 2 emission intensity. Humification was measured by changes in the share of structural fragments in organic matter of litter from solid-state 13 C NMR. We found logarithmic relationship between the rate of carbon mineralization and initial C:N ratio in litter, having maximum at C:N ratio of 22. Mineral nitrogen treatment increased the intensity of mineralization of the litter fractions poor in nitrogen (C:N ratio exceeding 66) and inhibited CO 2 emission from decomposition of litter with high nitrogen content (C:N ratio from 9 to 32). During the litter decomposition the Alkyl/O-Alkyl ratio increased. It corresponds to the level of humification of plant matter in soils. Additional nitrogen treatment has stimulated humification, especially during pine needles decomposition. Thus we found the effect of endogenous and mineral nitrogen on both mineralization and humification of forest litter. Acknowledgements: This study was financially supported by the Russian foundation for basic research (14-04-01738, 14-04-01884). Keywords: forest litter, plant debris decomposition, C:N ratio, mineralization, humification, mineral nitrogen. REFERENCES Aleksandrova L.N., Organicheskoe veshchestvo pochvy i protsessy ee transformatsii (Organic matter of soils and the soil transformation), Leningrad: Nauka, 1980, 287 p. Allison S.D., Lebauer D.S., Ofrecio M.R., Reyes R., Ta A.-M., Tran T.M., Low levels of nitrogen addition stimulate decomposition by boreal forest fungi, Soil biology and biochemistry , 2009, Vol. 41, No. 2, pp. 293-302. Averkieva I.Y., Priputina I.V., Otsenka vliyaniya tekhnogennoi emissii NOx na pitatel'nyi rezhim lesnykh biogeotsenozov Podmoskov'ya (Nitrogen oxides (NOx) technogenic emission influence on Moscow Region forest biogeocoenoses trophic regime assessment), Vestnik Kostromskogo gosudarstvennogo universiteta im. N.A. Nekrasova , 2011, Vol. 17, No. 3, pp. 51-57. Berg B., Decomposition patterns for foliar litter - A theory for influencing factors, Soil biology and biochemistry , 2014, Vol. 78, pp. 222-232. Carreiro M.M., Sinsabaugh R.L., Repert D.A., Parkhurst D.F., Microbial enzyme shifts explain litter decay responses to simulated nitrogen deposition, Ecology , 2000, Vol. 81, No. 9, pp. 2359-2365. Chernogaeva G.M., Peshkov Y.V., Kotlyakova M.G., Smirnov V.D., Obzor sostoyaniya i zagryazneniya okruzhayushchei sredy v Rossiiskoi Federatsii za 2013 god (Review of environmental conditions and pollution in the Russian Federation in 2013), Moscow: Rosgidromet, 2014, 228 p. Dijkstra F.A., Hobbie S.E., Knops J.M.H., Reich P.B., Nitrogen deposition and plant species interact to influence soil carbon stabilization, Ecology letters , 2004, Vol. 7, No. 12, pp. 1192-1198. Goldman E., Green L.H., Practical handbook of microbiology , Boca Raton: CRC Press, 2015, 1055 p. Gruber N., Galloway N., An Earth-system perspective of the global nitrogen cycle, Nature , 2008, Vol. 451, No. 7176, pp. 293-296. Hobbie S.E., Eddy W.C., Buyarski C.R., Adair E.C., Ogdahl M.L., Weisenhorn P., Response of decomposing litter and its microbial community to multiple forms of nitrogen enrichment, Ecological monographs , 2012, Vol. 82, No. 3, pp. 389-405. Knorr M., Frey S.D., Curtis P.S., Nitrogen additions and litter decomposition: a meta-analysis, Ecology , 2005, Vol. 86, No. 12, pp. 3252-3257. Kogel-Knabner I., The macromolecular organic composition of plant and microbial residues as inputs to soil organic matter, Soil biology and biochemistry , 2002, Vol. 34, No. 2, pp. 139-162. Larionova A.A., Zolotareva B.N., Kolyagin Y.G., Kvitkina A.K., Kaganov V.V., Kudeyarov V.N., Composition of structural fragments and the mineralization rate of organic matter in zonal soils, Eurasian soil science , 2015, Vol. 48, No. 10, pp. 1110-1119. Leppanen S.M., Salemaa M., Smolander A., Makipaa R., Tiirola M., Nitrogen fixation and methanotrophy in forest mosses along a N deposition gradient, Environmental and experimental botany , 2013, Vol. 90, pp. 62-69. Orlov D.S., Biryukova O.N., Sukhanova N.I., Organicheskoe veshchestvo pochv Rossiiskoi Federatsii (Organic matter in soils of the Russian Federation), Moscow: Nauka, 1996, 253 p. Pestriakov V.K., Kovsh N.V., Popov A.I., Chukov S.N., Modelirovanie transformatsii organicheskikh veshchestv v laboratornom eksperimente (Organic substances transformation modelling in a laboratory experiment), Pochvovedenie , 1990, No. 3, pp. 30-41. Prescott C.E., Litter decomposition: what controls it and how can we alter it to sequester more carbon in forest soils? , Biogeochemistry , 2010, Vol. 101, No. 1, pp. 133-149. Preston C.M., Nault J.R., Trofymow J.A., Chemical changes during 6 years of decomposition of 11 litters in some Canadian forest sites. Part 2. 13 C abundance, solid-state 13 C NMR spectroscopy and the meaning of ''lignin'', Ecosystems , 2009, Vol. 12, No. 7, pp. 1078-1102. Preston C.M., Nault J.R., Trofymow J.A., Smyth C., Anderson D., Camire C., Duchesne L., Fyles J., Kozak L., Kranabetter M., Moore T., Morrison I., Prescott C., Siltanen M., Zoltai S., Titus B., Visser S., Wein R., White D., Kutny L., Chemical changes during 6 years of decomposition of 11 litters in some Canadian forest sites. Part 1. Elemental composition, tannins, phenolics, and proximate fractions Ecosystems , 2009, Vol. 12, No. 7, pp. 1053-1077. Pryanishnikov D.N., Azot v zhizni rastenii i v zemledelii SSSR (Nitrogen and the plant life, and crop farming in the USSR), Moscow - Leningrad: Izd-vo AN SSSR, 1945, 199 p. Safonov S.S., Karelin D.V., Grabar V.A., Latyshev B.A., Grabovskii V.I., Uvarova N.E., Zamolodchikov D.G., V.N. K., Gitarskii M.L., Emissiya dioksida ugleroda ot razlozheniya valezha v yuzhnotaezhnom el'nike (The Emission of Carbon from the Decomposition of Woody Debris in the Southern Taiga Spruce Forest), Lesovedenie , 2012, No. 5, pp. 44-49. Semenov V.M., Ivannikova L.A., Kuznetsova T.V., Semenova N.A., The role of plant biomass in the formation of the active pool of soil organic matter, Eurasian soil science , 2004, Vol. 37, No. 11, pp. 1196-1204. Sutton M.A., Howar C.M., Erisman J.W., Billen G., Bleeker A., Grennfelt P., Van Grinsven H., Grizzetti B., The European nitrogen assessment: sources, effects and policy perspectives , New York: Cambridge University Press, 2011, 664 p. Umarov M.M., Kurakov A.V., Stepanov A.L., Mikrobiologicheskaya transformatsiya azota v pochve (Microbial transformation of nitrogen in soils), Moscow: GEOS, 2007, 137 p. Vedrova E.F., Intensivnost' razlozheniya organicheskogo veshchestva na poverkhnosti i v tolshche pochvy (The intensity of organic matter decomposition at the surface and in the soil), In: Lesnye ekosistemy Eniseiskogo meridiana (Forest ecosystems of the Yenissei meridian), Novosibirsk: Izd-vo SO RAN, 2002, pp. 231-248 (356 p.). Vedrova E.F., Organic matter decomposition in forest litters, Eurasian soil science , 1997, Vol. 30, No. 2, pp. 216-223. Zhang D., Hui D., Luo Y., Zhou G., Rates of litter decomposition in terrestrial ecosystems: global patterns and controlling factors, Journal of plant ecology , 2008, Vol. 1, No. 1, pp. 85-93.
Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.
Comment cette classification a été obtenuedéplier
Prédiction machine sur la base complète
Imitation des enseignantsNi prévalence calibrée, ni vérité terrain. Validation humaine à venir. Le volet Gemma est une étiquette directe du modèle pour chaque travail de la base, lue sur la notice réduite au titre. Le volet Codex est un classifieur appris des 10 348 étiquettes directes de Codex et calibré sur les taux pondérés de l'échantillon; les champs sans appui suffisant ne portent aucun appel Codex. Le mode candidate est l'union des deux volets; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont pas des étiquettes humaines.
Scores du classifieur distillé par catégorie (deux têtes)
| Catégorie | Codex | Gemma |
|---|---|---|
| Métarecherche | 0,000 | 0,001 |
| Méta-épidémiologie (sens strict) | 0,000 | 0,000 |
| Méta-épidémiologie (sens large) | 0,000 | 0,000 |
| Bibliométrie | 0,001 | 0,001 |
| Études des sciences et des technologies | 0,001 | 0,001 |
| Communication savante | 0,002 | 0,001 |
| Science ouverte | 0,000 | 0,001 |
| Intégrité de la recherche | 0,000 | 0,001 |
| Charge utile insuffisante (le modèle a refusé de juger) | 0,008 | 0,002 |
Scores machine (provisoires)
Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.
Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.
score_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découleClassification
machine, non validéePrédiction automatique; un appel candidat d’une seule source (Gemma direct ou Codex distillé), pas un consensus.
Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».