Post-Fire State of Taiga Soils and Vegetation of the Khamar-Daban Range (Cisbaikalia)
We have studied a naturally burnt forest in the Baikalsky State Nature Biosphere Reserve within the basin of the Mishikha River in the belt of dark-coniferous fir ( Abies sibirica ) taiga with Siberian pine ( Pinus sibirica ) on ferruginated stony burozems (Skeletic Cambisols (Humic, Protospodic)) a...
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| Veröffentlicht in: | Eurasian soil science 2022-09, Vol.55 (9), p.1196-1208 |
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| creator | Koshovskii, T. S. Gennadiev, A. N. Gamova, N. S. Faronova, E. A. Yazrikova, T. E. |
| description | We have studied a naturally burnt forest in the Baikalsky State Nature Biosphere Reserve within the basin of the Mishikha River in the belt of dark-coniferous fir (
Abies sibirica
) taiga with Siberian pine (
Pinus sibirica
) on ferruginated stony burozems (Skeletic Cambisols (Humic, Protospodic)) and ferruginated metamorphosed lithozems (Cambic Leptosols (Humic, Protospodic)) in a habitat typical for mid-mountains of the northern macroslope of the Khamar-Daban Range. Changes in the soil and plant cover on the burnt plot have been compared with the background undisturbed forest landscape. The structure of the post-fire plant community has been significantly changed and simplified. The thickness of litter-peat horizons has decreased, new pyrogenic horizons have appeared, the concentration of labile carbon, ammonium, and labile nitrogen has dropped, and the content of labile phosphorus has increased. The total content of polycyclic aromatic hydrocarbons (PAH) has decreased after the fire due to the burnout of organic matter, adsorbing polyarenes. The content of a group of high-molecular weight PAHs in soils has significantly increased under the effect of fire. |
| doi_str_mv | 10.1134/S1064229322090101 |
| format | Article |
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Abies sibirica
) taiga with Siberian pine (
Pinus sibirica
) on ferruginated stony burozems (Skeletic Cambisols (Humic, Protospodic)) and ferruginated metamorphosed lithozems (Cambic Leptosols (Humic, Protospodic)) in a habitat typical for mid-mountains of the northern macroslope of the Khamar-Daban Range. Changes in the soil and plant cover on the burnt plot have been compared with the background undisturbed forest landscape. The structure of the post-fire plant community has been significantly changed and simplified. The thickness of litter-peat horizons has decreased, new pyrogenic horizons have appeared, the concentration of labile carbon, ammonium, and labile nitrogen has dropped, and the content of labile phosphorus has increased. The total content of polycyclic aromatic hydrocarbons (PAH) has decreased after the fire due to the burnout of organic matter, adsorbing polyarenes. The content of a group of high-molecular weight PAHs in soils has significantly increased under the effect of fire.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229322090101</identifier><language>eng</language><publisher>Moscow: Pleiades Publishing</publisher><subject>Abies sibirica ; Ammonium ; Ammonium compounds ; Aromatic compounds ; Aromatic hydrocarbons ; Biosphere ; Burnout ; Earth and Environmental Science ; Earth Sciences ; Fires ; Genesis and Geography of Soils ; Geotechnical Engineering & Applied Earth Sciences ; Molecular weight ; Mountains ; Organic matter ; Peat ; Phosphorus ; Pine trees ; Pinus sibirica ; Plant communities ; Plant cover ; Polycyclic aromatic hydrocarbons ; Soil ; Soils ; Taiga</subject><ispartof>Eurasian soil science, 2022-09, Vol.55 (9), p.1196-1208</ispartof><rights>Pleiades Publishing, Ltd. 2022. ISSN 1064-2293, Eurasian Soil Science, 2022, Vol. 55, No. 9, pp. 1196–1208. © Pleiades Publishing, Ltd., 2022. Russian Text © The Author(s), 2022, published in Pochvovedenie, 2022, No. 9, pp. 1098–1111.</rights><rights>COPYRIGHT 2022 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c307t-b1f5dee276c421cb790cdc29ef6bf0b59658b6a329915f8512e3038cb55b71543</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1064229322090101$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1064229322090101$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Koshovskii, T. S.</creatorcontrib><creatorcontrib>Gennadiev, A. N.</creatorcontrib><creatorcontrib>Gamova, N. S.</creatorcontrib><creatorcontrib>Faronova, E. A.</creatorcontrib><creatorcontrib>Yazrikova, T. E.</creatorcontrib><title>Post-Fire State of Taiga Soils and Vegetation of the Khamar-Daban Range (Cisbaikalia)</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>We have studied a naturally burnt forest in the Baikalsky State Nature Biosphere Reserve within the basin of the Mishikha River in the belt of dark-coniferous fir (
Abies sibirica
) taiga with Siberian pine (
Pinus sibirica
) on ferruginated stony burozems (Skeletic Cambisols (Humic, Protospodic)) and ferruginated metamorphosed lithozems (Cambic Leptosols (Humic, Protospodic)) in a habitat typical for mid-mountains of the northern macroslope of the Khamar-Daban Range. Changes in the soil and plant cover on the burnt plot have been compared with the background undisturbed forest landscape. The structure of the post-fire plant community has been significantly changed and simplified. The thickness of litter-peat horizons has decreased, new pyrogenic horizons have appeared, the concentration of labile carbon, ammonium, and labile nitrogen has dropped, and the content of labile phosphorus has increased. The total content of polycyclic aromatic hydrocarbons (PAH) has decreased after the fire due to the burnout of organic matter, adsorbing polyarenes. The content of a group of high-molecular weight PAHs in soils has significantly increased under the effect of fire.</description><subject>Abies sibirica</subject><subject>Ammonium</subject><subject>Ammonium compounds</subject><subject>Aromatic compounds</subject><subject>Aromatic hydrocarbons</subject><subject>Biosphere</subject><subject>Burnout</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fires</subject><subject>Genesis and Geography of Soils</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Molecular weight</subject><subject>Mountains</subject><subject>Organic matter</subject><subject>Peat</subject><subject>Phosphorus</subject><subject>Pine trees</subject><subject>Pinus sibirica</subject><subject>Plant communities</subject><subject>Plant cover</subject><subject>Polycyclic aromatic hydrocarbons</subject><subject>Soil</subject><subject>Soils</subject><subject>Taiga</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNp1kMFPwyAUxhujiXP6B3gj8aKHTh6UthyX6dRoonGb8dYAhY7ZlQndwf9elpl4MIbDI3zf7_HelyTngEcANLueAc4zQjglBHMMGA6SATCWp8DZ-2G8Rznd6cfJSQgrjGlZZuUgWby40KdT6zWa9aLXyBk0F7YRaOZsG5DoavSmGx0167qd2i81elyKtfDpjZCiQ6-iazS6nNgghf0QrRVXp8mREW3QZz91mCymt_PJffr0fPcwGT-liuKiTyUYVmtNilxlBJQsOFa1IlybXBosGc9ZKXNBCefATMmAaBoHV5IxWQDL6DC52PfdePe51aGvVm7ru_hlRaKB0BJyiK7R3tWIVle2M673QsVT67VVrtPGxvdxASXmJWQ0ArAHlHcheG2qjbdx4a8KcLWLu_oTd2TIngnRGwPxv6P8D30DrJd-ew</recordid><startdate>20220901</startdate><enddate>20220901</enddate><creator>Koshovskii, T. 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S.</creatorcontrib><creatorcontrib>Gennadiev, A. N.</creatorcontrib><creatorcontrib>Gamova, N. S.</creatorcontrib><creatorcontrib>Faronova, E. A.</creatorcontrib><creatorcontrib>Yazrikova, T. 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S.</au><au>Gennadiev, A. N.</au><au>Gamova, N. S.</au><au>Faronova, E. A.</au><au>Yazrikova, T. E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Post-Fire State of Taiga Soils and Vegetation of the Khamar-Daban Range (Cisbaikalia)</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2022-09-01</date><risdate>2022</risdate><volume>55</volume><issue>9</issue><spage>1196</spage><epage>1208</epage><pages>1196-1208</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>We have studied a naturally burnt forest in the Baikalsky State Nature Biosphere Reserve within the basin of the Mishikha River in the belt of dark-coniferous fir (
Abies sibirica
) taiga with Siberian pine (
Pinus sibirica
) on ferruginated stony burozems (Skeletic Cambisols (Humic, Protospodic)) and ferruginated metamorphosed lithozems (Cambic Leptosols (Humic, Protospodic)) in a habitat typical for mid-mountains of the northern macroslope of the Khamar-Daban Range. Changes in the soil and plant cover on the burnt plot have been compared with the background undisturbed forest landscape. The structure of the post-fire plant community has been significantly changed and simplified. The thickness of litter-peat horizons has decreased, new pyrogenic horizons have appeared, the concentration of labile carbon, ammonium, and labile nitrogen has dropped, and the content of labile phosphorus has increased. The total content of polycyclic aromatic hydrocarbons (PAH) has decreased after the fire due to the burnout of organic matter, adsorbing polyarenes. The content of a group of high-molecular weight PAHs in soils has significantly increased under the effect of fire.</abstract><cop>Moscow</cop><pub>Pleiades Publishing</pub><doi>10.1134/S1064229322090101</doi><tpages>13</tpages></addata></record> |
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| subjects | Abies sibirica Ammonium Ammonium compounds Aromatic compounds Aromatic hydrocarbons Biosphere Burnout Earth and Environmental Science Earth Sciences Fires Genesis and Geography of Soils Geotechnical Engineering & Applied Earth Sciences Molecular weight Mountains Organic matter Peat Phosphorus Pine trees Pinus sibirica Plant communities Plant cover Polycyclic aromatic hydrocarbons Soil Soils Taiga |
| title | Post-Fire State of Taiga Soils and Vegetation of the Khamar-Daban Range (Cisbaikalia) |
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