![]() Address: Naberezhnaya Severnoy Dviny, 17, Arkhangelsk, 163002, Russian Federation, Northern (Arctic) Federal University named after M.V.Lomonosov, office 1425
Phone: +7 (8182) 21-61-18 Lesnoy Zhurnal |
V.V. Polyakova Complete text of the article:Download article (pdf, 0.4MB )UDС631.4:631.811.944DOI:10.17238/issn0536-1036.2015.3.29AbstractIron is an microelement, involved in the process of photosynthesis. Its scarcity or excess affects negatively on plants growth. High content of bivalent ferrous oxide in ground water can exert the clogging of drain lines on drain territories by ferrous precipitation, that nega-tively affect on hydrologic conditions of plants growth. There is observed abundant red fer-ruginous sediment in open channels in the park of the Forestry University. In groundwater general and bivalent iron more than in pond water. Ground stream get through mineral and species, contained iron, that import iron in water, and pond water is with an atmospheric condensation. In groundwater, located close to the surface of the earth, bivalent iron is more, than in water at a greater depth. There is seasonal dynamics of bivalent iron in groundwater. The concentration of bivalent iron in groundwater is optimal for normal growth and devel-opment of plants. By the end of vegetation period occurred silting of drainage pipes by 40 %. This violates the hydrological conditions of growth and development of plants.AuthorsV.V. Polyakova, Postgraduate StudentAffiliationSaint Petersburg State Forest Technical University named under S.M. Kirov, Institutskiy per., 5, Saint-Petersburg, 19402, Russia; е-mail: v.v.p.i53@bk.ruKeywordsgeneral iron, bivalent iron, underground water, park of Forestry University.References1. Knipovich Yu.N., Morachevskii Yu.V. Analiz mineral'nogo syr'ya [Analysis of Mineral Raw Material]. Leningrad, 1956. 1056 p. 2. Vodyanitskiy Yu.N. Khimiya i minerologiya pochvennogo zheleza [Chemistry and Mineralogy of the Soil Iron]. Moscow, 2002. 236 p. 3. Vozbutskaya A. E. Khimiya pochvy [The Chemistry of the Soil]. Moscow, 1968. 428 p. 4. Dobrynin Yu.A. Veroyatnostnye modeli protsessov zaileniya osushitel'nykh kanalov gidromeliorativnykh sistem [Probabilistic Models of Silting Processes of Drainage Channels of Reclamation Systems]. Izvestiya Sankt-Peterburgskoy lesotehnicheskoy akade-mii, Saint-Petersburg, 2007, no. 180, pp. 103–110. 5. Zonn S.V. Zhelezo v pochvakh (geneticheskie i geograficheskie aspekty) [Iron in Soils (Genetic and Geographical Aspects)]. Moscow, 1982, no. 9. 208 p. 6. Ilyaletdinov A.N. Biologicheskaya mobilizatsiya mineral'nykh soedineniy [Biolog-ical Mobilization of Mineral Compounds]. Alma-Ata, 1966. 332 p. 7. Kitaeva L.I. Svyaz' mezhdu soderzhaniem zheleza, tsinka, margantsa, kolich-estvom gumusa i kislotnost'yu v pochvakh Penzenskoy oblasti [The Relationship Between the Concentrations of Iron, Zinc, Manganese, Quantity of Humus and Acidity in the Soil of the Penza region]. Pochvovedenie, Moscow, 1990, pp. 132–135. 8. Kulikova V.K. Sezonnye izmeneniya khimicheskikh svoystv podzolistykh peschanykh pochv [Seasonal Changes of the Chemical Properties of Podzolic Soils]. Pochvy sosnovykh lesov Karelii [Soils of Pine Forests in Karelia]. Petrozavodsk, 1978, pp. 71–85. 9. Lir Kh., Pol'ster G., Fidler G.N. Fiziologiya drevesnykh rasteniy [Physiology of Woody Plants]. Moscow, 1974. 424 p. 10. Matinyan N.N., Myshkina I.V., Nemchinova I.A. Ekologicheskie usloviya zaokhrivaniya drenazhnykh system Nemanskoy nizmennosti [Ecological Conditions of Drainage Systems Soiling in the Neman Lowland]. Ekologo-geneticheskie issledovaniya pochv v gumidnykh landshaftakh [Ecological and Genetic Researches of Soils in Humid Landscapes: Collected Papers]. Saint-Petersburg, 1996, pp. 3–18. 11. Morozova R.M. Pochvoobrazovanie na peschanykh otlozheniyakh Karelii [Soil Formation on Sandy Sediments of Karelia]. Pochvy sosnovykh lesov Karelii [Soils of Pine Forests in Karelia]. Petrozavodsk, 1978, pp. 4–43. 12. Motuzova G.V., Degtyareva A.K. Formy soedineniy zheleza v pochvennykh rastvorakh i drenazhnykh vodakh na primere Yakhromskoy poymy [Forms of Iron Com-pounds in the Soil Solutions and Drainage Waters on the Example of Yakhroma Flood-plain]. Pochvovedenie, Moscow, 1993, no.1, pp. 110–114. 13. Rin'kis G.Ya. Znachenie vzaimovliyaniya elementov v optimizatsii mineral'nogo pitaniya rasteniy [The Value of the Interaction of Elements in the Optimization of the Min-eral Nutrition of Plants]. Mikroelementy v komplekse mineralnogo pitaniya rasteniy [Micro-elements in the Complex of Mineral Nutrition of Plants]. Riga, 1975, pp. 16–28. 14. Rukovodstvo po analizu vody. Pit'evaya i prirodnaya voda, pochvennye vytyazhki [Manual on Analysis of Water. Drinking and Natural Water, Soil Extraction]. Saint-Petersburg, 2012. 264 p. 15. Yakovlev S.A. Geologicheskoe stroenie mestnosti parka Lesnogo Instituta [Ge-ology of the Area of the Park Forest Institute]. Izvestiya Leningradskogo Lesnogo Instituta, Lelingrad, 1929, no. 37, pp. 219–235.Iron in the Surface and Ground Waters |
Make a Submission
Lesnoy Zhurnal (Russian Forestry Journal) was awarded the "Seal of Recognition for Active Data Provider of the Year 2024" INDEXED IN:
|
![]() |
|
![]() |
![]() |
![]() |
|
![]() |
|
![]() |
|
![]() |
|
![]() |
![]() |
![]() |
|
![]() |
![]() |
![]() |
|
![]() |
![]() |
![]() |
|
![]() |
![]() |
![]() |
|
![]() |
|
![]() |
![]() |
![]() |
![](/img/transparent.gif)