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Ninth International Conference on Permafrost ... - IARC Research

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1970 2005Repeated Mapping of the Northern Taiga Ecosystems in West Siberia, Disturbed byPipeline C<strong>on</strong>structi<strong>on</strong>E.V. UstinovaEarth Cryosphere Institute, Tyumen, RussiaEngineering c<strong>on</strong>structi<strong>on</strong> in the north of West Siberialeads to disturbances of vegetati<strong>on</strong> cover and changingpermafrost c<strong>on</strong>diti<strong>on</strong>s. The scale of changes is in directrelati<strong>on</strong> to the degree of human-induced disturbanceand landscape properties. Many natural features can be lostunder increasing anthropogenic pressure; therefore, solvingthe problem of rati<strong>on</strong>al land usage and wildlife managementbecomes extremely difficult. The informati<strong>on</strong> presented hereresults from ecosystem m<strong>on</strong>itoring.M<strong>on</strong>itoring of disturbed ecosystems has been carriedout for 35 years al<strong>on</strong>g a gas pipeline located in the subz<strong>on</strong>eof northern taiga at the Nadym field stati<strong>on</strong>. Terrainchanges are studied every 3–5 years by large-scale repeatedmapping of the territory, using c<strong>on</strong>temporary air photos andfieldwork. The last analyses were made in 2006. The greatestenvir<strong>on</strong>mental disturbances occurred during pipelinec<strong>on</strong>structi<strong>on</strong> in 1971–1972 and pipeline replacement in2004. Smaller changes took place in 1974 in relati<strong>on</strong> toelectrical line c<strong>on</strong>structi<strong>on</strong>, and in 1983, in adding new fillto the embankment. The service road al<strong>on</strong>g the pipeline isrec<strong>on</strong>structed every year.Disturbance of natural c<strong>on</strong>diti<strong>on</strong>s triggered activati<strong>on</strong> ofthermokarst and frost heave. Bog formati<strong>on</strong> in areas p<strong>on</strong>dedby embankments and wind erosi<strong>on</strong> of sand <strong>on</strong> dry sites alsotake place. Observati<strong>on</strong>s show that in disturbed areas theoccurrence of lakes has increased 22%.The landscape hierarchy was described accordingto Melnikov (1983) using informati<strong>on</strong> <strong>on</strong> permafrostdistributi<strong>on</strong>, topography, and vegetati<strong>on</strong>. A series of digitalmaps shows natural terrain units (ecosytems) as well asterrain units affected by c<strong>on</strong>structi<strong>on</strong> over the time periodfrom 1970 to 2006. These maps are based <strong>on</strong> air photographyof different years and <strong>on</strong> field surveys. The locati<strong>on</strong> ofm<strong>on</strong>itoring sites, temperature boreholes, and features relatedto сryogenic processes are shown as well. The database ofboreholes is linked to the maps.The analysis of the maps compiled for differentyears revealed changes in the area of human-induceddisturbances and trends in ecosystem development underthe impact of climatic changes and disturbances (Fig.1). After c<strong>on</strong>structi<strong>on</strong>, the width of the disturbance z<strong>on</strong>eincreased differently in the various terrains. The increase inboggy areas due to swamping of the forest ecosystems wasdetermined by comparing the maps of 1970 with those of1988 (Fig. 1).During 2004 pipeline rec<strong>on</strong>structi<strong>on</strong>, pipes were replaced.The histogram (Fig. 2) is based <strong>on</strong> comparis<strong>on</strong> of the terrainmap of 1970, which was prepared prior to c<strong>on</strong>structi<strong>on</strong> ofa gas pipeline, and the map of 2005. Figure 2 shows thathuman-induced disturbance has caused an increase of 2.9%25201510504 16 19 20 23 45 46 48 49 50 60 61 72 100 .1970 1988Figure1: Frequency of ecosystems at the Nadym site in 1970 and1988 years.4 - dry gentle slopes with birch-pine-cowberry-lichen sparseforests; 16 - flat slightly drained sites with birch-pine-wildrosemary-lichen–moss sparse forests; 19 - flat boggy sites withlarch-wild rosemary-moss open forests; 20 - flat boggy sites withhummocky larch-wild rosemary-lichen-moss open forests; 23- peat-mineral frost mounds with sedge-shrub lichen-moss openlarch-pine woodland; 45 - hollows with sedge-moss mires; 46 -hollows and flat sites with tussocky sedge-moss mires; 48 - flatsites with hummocky sedge-peat moss bogs; 49 - flat sites withdwarf shrub-sedge-peat moss bogs; 50 - hollows occupied bogswith dwarf shrub-sedge-peat moss ridges and sedge-moss pools;60 - flat sites with cloudberry-wild rosemary-moss- peatlands, 61- flat sites with cloudberry-wild rosemary-moss-lichen peatlands;72 - palsa peatland with sedge-shrub-moss-lichen cover <strong>on</strong> palsaand sedge-peat moss <strong>on</strong> pools between palsa; 100 - flat siteswith hummocky tundras with sedge-shrub-moss-lichen cover <strong>on</strong>hummocks and sedge-peat moss <strong>on</strong> pools and rare frost boils; 03- lakes.in the area of hummocky sites (ecosystem 100), 1.8% in theareas of bogs (ecosystems 45, 46, 48), and 1.5% in the area ofpalsa peatland (ecosystem 72). Some flat areas (ecosystems60 and 61) have partly recovered, however, and disturbancedecreased by 2.8%.Most disturbance relates to the removal of vegetati<strong>on</strong>,modificati<strong>on</strong> of a microrelief, removal of 10 to 20 cm of peatduring clearing of the right-of-way, and partial destructi<strong>on</strong>of vegetati<strong>on</strong> as a result of road transportati<strong>on</strong>. The smallerareas occupy the sites disturbed as a result of caterpillartransport travel, where vegetati<strong>on</strong>, soil cover, and microreliefhave been broken <strong>on</strong>ly in part. The areas occupied by sites325

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