Вестник Кольского научного центра РАН. 2015, №1.

CONTENTS Authors Valery I. Diomin - scientific researcher of Polar Geophysical Institute KSC RAS; e-mail: demin@pgia.ru Aleksandra R. Antsiferova - meteorologist of Murmansk Administration on Hydrometeorology and Environmental Monitoring; e-mail: klimat@kolgimet.ru Olga I. Mokrotovarova - Chief of Murmansk Administration on Hydrometeorology and Environmental Monitoring; e-mail: leader@kolgimet.ru LITERATURA 1. Demin V.I. Osnovnye klimaticheskie tendencii na Kol'skom poluostrove za period instrumental'nyh meteorologicheskih nablyudenij // Trudy KNC RAN. "Prikladnaya ehkologiya Severa". 2012. 2 (9). Apatity, 2012. S. 98-110. 2. Rubinshtejn E.S. Klimat SSSR. CH. 1. Temperatura vozduha. Vyp. 2. Srednie mesyachnye temperatury vozduha v Evropejskoj chasti SSSR za otdel'nye gody s sevra do 55 s.sh. L.: GGO, 1929. 180 s. 3. Yakovlev B.A. Klimat Murmanska. L.: Gidrometeoizdat, 1972, 108 s. 4. Spravochnik po klimatu SSSR. L., Gidrometeoizdat, 1965. Vyp. 2, ch. 1. 144 s. 5. Kobysheva N.V., Narovlyanskij G.YA. Klimatologicheskaya obrabotka meteorologicheskoj informacii. L.: Gidrometeoizdat, 1978. 296 s. 6. Metody klimatologicheskoj obrabotki meteorologicheskih nablyudenij / pod red. O.A. Drozdova. L.: Gidrometeoizdat, 1957. 492 s. 7. Demin V.I. Neklimaticheskie klimaticheskie izmeneniya // Materialy glyaciologicheskih issledovanij. 2012. № 1. S. 110-114. 8. Andresen L. Homogenization of monthly long-term temperature series of mainland Norway. Met.no. Note 2, 2011. Norwegian Meteorological Institute, Oslo, Norway. Rezhim dostupa: http: //met.no/filestore/Homog_Norway.pdf 9. Klingbjer P. and Moberg A. A composite monthly temperature record from Tornedalen in northern Sweden, 1802-2002, Int. Journal of Climatology, 2003. 23:1465-1494. 10. Lobanov V.A., Smirnov I.A., SHadurskij A.E. Praktikum po klimatologii. CHast' 1: uchebnoe posobie. Spb.: RGGMU, 2011. 145 s. 11. Svod pravil po proektirovanie i stroitel'stvu: SP 33-101­ 2003. Opredelenie osnovnyh raschetnyh gidrologicheskih harakteristik. M.,: 2004. 12. Semenov A.V. Instrumental'nye klimaticheskie nablyudeniya na Kol'skom poluostrove i osobennosti obsluzhivaniya regional'nyh potrebitelej klimaticheskoj informaciej // doklad na Mezhd. konferencii «Adaptaciya k izmeneniyu klimata i ee rol' v obespechenii ustojchivogo razvitiya regionov», Murmansk, 13 maya 2008 g. // Rezhim dostupa: http://www.myshared.ru/slide/378692 13. Climate changes 2014. Physical bases. Fifth Assessment Report. Rezhim dostupa: http://www.ipcc.ch/report/ar5. 14. Hromov S.P., Mamontova L.I. Meteorologicheskij slovar'. L.: Gidrometeoizdat, 1974. 568 s. 15. Girs A.A. Makrocirkulyacionnyj metod dolgosrochnyh meteorologicheskih prognozov. L.: Gidrometeoizdat, 1974. 488 s. 16. Demin V.I., Svyashchennikov P.N., Ivanov B.V. Izmeneniya krupnomasshtabnoj cirkulyacii atmosfery i sovremennoe poteplenie klimata na Kol'skom p-ove // Vestnik KNC RAN. T.84. №2, S. 101-105. 17. Oke T.R. Klimaty pogranichnogo sloya. L.: Gidrometeoizdat, 1982. 360 s. 18. Mikroklimat SSSR / pod red. I.A. Gol'cberg. L., Gidrometeoizdat, 1967. 286 s. 19. Mishchenko Z.A. Bioklimat dnya i nochi. L., Gidrometeoizdat, 1984. 280 s. V.A. Myazin DETERMINATION OF HYDROCARBONS AND PRODUCTS OF THEIR TRANSFORMATION AT POLLUTION OF CULTIVATED PODZOLIC SOILS IN THE EURO-ARCTIC REGION The article discusses assessment of soil contamination by hydrocarbons and products of their transformation. A comparative analysis of the contaminated soil was carried out by two ways, namely IR spectroscopy and separation of the chloroform bitumoid. It is shown that increasing of pollution period as well as cleaning and recovery of soil (application of mineral and organic fertilizers or bacterial preparations) results in a redistribution of the components of the soil bitumoid. Quantity of petroleum hydrocarbons, determined by IR spectroscopy goes down, while quantity of products of their transformation increases. Moreover, some of these products may negatively affect the soil. After 3 years of contamination, content of the products of transformation for hydrocarbons can reach 90% of the organic matter of the soil bitumoid. That is why the extent of residual contamination cannot be fully assessed by using IR spectroscopy only, without additional research. Keywords: oil, soil bitumoid, bioremediation, cultivated podzolic soil. 184 Herald o fKola Science Centre o f the Russian Academy o f Sciences 1/2005(20)