Soil susceptibility on reduction as an index of soil properties applied in the investigation upon soil devastation

• Autorzy: Labuda S. , Vetchinnikov A.

Warianty tytułu

PL

Podatność gleby na redukcję jako wskaźnik właściwości gleby zastosowany w badaniach nad dewastacją gleby

• Języki publikacji: EN

Abstrakty

EN

The investigations were conducted on the soil samples taken from two localities on two objects: the cultivated soils and the devastated soils caused by building of oil pipelines near Nizhniy Novgorod, Russia. Measurements of redox potential were conducted in soil suspension at the soil to water ratio as 1:1 under the standard laboratory conditions. The soil susceptibility on reduction (SSR) index define the decrease of redox potential in time on one day of incubation and expressed in mV per day. Conducted investigations showed the soil susceptibility on reduction indices had been counted in three ways were significantly diverse, both between studied soils as also between the soils devastation. The soil susceptibility on reduction index can be considered as the useful and universal index of soil fertility or soil quality, too. Determination of the soil susceptibility on reduction can be the easy and practically useful method in the investigations of soils, because the simple measurements of redox potential may be execute two times only, the first measurement after preparing the soil suspension and the second measurement in the last day of incubation accepting, at the first day of soil suspension preparation and the last day of measurements enough just a week.

PL

Badania przeprowadzono na próbkach glebach pobranych w dwóch miejscowości na dwóch obiektach gleb uprawnych i gleb zdewastowanych przez budowę rurociągów koło Niżnego Nowgorodu w Rosji. Pomiary potencjału redoks zostały wykonane w wodnej zawiesinie glebowej przy stosunku gleba:woda jak 1:1 w standardowych warunkach laboratoryjnych. Wskaźnik podatności gleby na redukcję (SSR) określa spadek potencjału redoks w czasie na jeden dzień inkubacji i wyrażony był w mV na dobę. Przeprowadzone badania wykazały, że podatność gleby na redukcję obliczona trzema sposobami była znacząco zróżnicowana zarówno między badanymi glebami, jak też między glebami zdewastowanymi. Wskaźnik podatności gleby na redukcję może być rozważany jako przydatny i uniwersalny wskaźnik żyzności gleby lub jakości gleby. Określanie podatności gleby na redukcję może być łatwą i praktycznie przydatną metodą w badaniach gleb, gdyż pomiary potencjału redoks w wodnej zawiesinie glebowej przeprowadza się tylko dwa razy, pierwszy raz po sporządzeniu zawiesiny glebowej i drugi raz w ostatnim dniu inkubacji, przyjmując, że te pomiary można wykonać w jednym tygodniu.

Słowa kluczowe

EN

Russian Federation; soil redox potential; soil susceptibility on reduction; soil devastation

PL

Federacja Rosyjska; potencjał redoks w glebie; podatność gleby na redukcję; dewastacja gleb

• Wydawca: Towarzystwo Chemii i Inżynierii Ekologicznej
• Czasopismo: Ecological Chemistry and Engineering. S
• Rocznik: 2011
• Tom: Vol. 18, nr 3
• Strony: 333--344
• Opis fizyczny: Bibliogr. 41 poz., rys.

Twórcy

autor

Labuda S.

autor

Vetchinnikov A.

• Department of Agricultural and Environmental Chemistry, Lublin University of Natural Sciences, ul. Akademicka 15, 20-033 Lublin,

Bibliografia

• [1] Bartlett R.J. and James B.R.: Redox chemistry in soils. Adv. Agron., 1993, 10, 151-208.
• [2] Bohn H.L.: Redox potentials. Soil Sci., 1971, 112(1), 39-45.
• [3] Fiedler S., Vepraskas M.J. and Richardson J.L.: Soil redox potential, importance, field measurements, and observations. Adv. Agron., 2007, 94, 1-54.
• [4] Jeffery J.W.O.: Measuring the state of reduction of a waterlogged soil. J. Soil Sci., 1961, 12(2), 317-325.
• [5] Patrick W.H. and Fontenot W.J.: Growth and mineral composition of rice at various soil moisture tensions and oxygen levels. Agron. J., 1976, 68(2), 325-329.
• [6] Patrick Jr., W.H.: Extractable iron and phosphorus in a submerged soil at controlled redox potentials. Proc. the 8th Int. Congress of Soil Sci., Bucharest, Romania 1964, 4, 605-609.
• [7] Rabenhorst M.C., Hively W.D. and James B.R.: Measurements of soil redox potential. Soil Sci. Soc. Amer. J., 2009, 73(2), 668-674.
• [8] Sommers L.E. and Lindsay W.L.: Effect of pH and redox on predicted heavy metal-chelate equilibria in soils. Soil Sci. Soc. Amer. J., 1979, 43(1), 39-47.
• [9] Tabatabai L.B. and Walker H.W.: Oxidation-reduction potential and growth of Clostridium perfringens and Pseudomonas fluorescens. Appl. Microbiol., 1970, 20(3), 441-446.
• [10] Bartlett R.J. and James B.R.: System for categorizing soil redox status by chemical field testing. Geoderma, 1995, 68(3), 211-218.
• [11] David R.: Determining redox system in lakes and rivers; thermodynamic interpretation of insitu measurements with a platinum electrode. Radiat. Environ. Biophys., 1986, 25(3), 219-229.
• [12] Gao S., Tanji K.K., Scardaci S.C. and Chow A.T.: Comparison of redox indicators in paddy soil during rice growing season. Soil Sci. Soc. Amer. J., 2002, 66(3), 805-817.
• [13] Herbel M.J., Suarez D.L., Goldberg S. and Gao S.: Evaluation of chemical amendments for pH and redox stabilization in aqueous suspensions of three California soils. Soil Sci. Soc. Amer. J., 2007, 71(3), 927-939.
• [14] Masscheleyn P.H., Delaune R.D. and Patrick W.H., Jr.: Effect of redox potential and pH on arsenic speciation and solubility in a contaminated soil. Environ. Sci. Technol., 1991, 25(8), 1414-1419.
• [15] Patrick W.H. and Turner F.T.: Effect o redox potential on manganese transformation in waterlogged soil. Nature, 1968, 220(5166), 476-478.
• [16] Smith J.H. Gilbert R.G. and Miller J.B.: Redox potentials and denitrification in a cropped potato processing waste water disposal field. J. Environ. Qual., 1976, 5(4), 397-399.
• [17] Snakin V.V. and Prisyazhnaya A.A.: Quantitative assessment of the degree of anthropogenic changes in soil by analyzing the in situ composition of the soil liquid phase. Geoderma, 1997, 75(¾), 279-287.
• [18] Tanji K.K., Gao S., Scardaci S.C. and Chow A.T.: Characterizing redox status of paddy soils with incorporated rice straw. Geoderma, 2003, 114(¾), 333-353.
• [19] Unger I.M., Muzika R.M., Motavall, P.P. and Kabrick J.: Evaluation of continuous in situ monitoring of soil changes with varying flooding regimes. Commun. Soil Sci. Plant Anal., 2008, 39(11&12), 1600-1619.
• [20] Yamane I. and Sato K.: Initial rapid drop of oxidation-reduction potential in submerged air-dried soils. Soil Sci. Plant Nutr., 1968, 14(2), 68-72.
• [21] Carter C.E.: Redox potential and sugarcane yield relationship. Trans. ASAE, 1980, 23(4), 924-927.
• [22] Labuda S.: Plant elemental compositions as affected by the soil oxygen stress. Probl. Agrofizyki, 1987, 52, 1-84 (in Polish).
• [23] Meek D.B. and Grass L.B.: Redox potential in irrigated desert soils as in indicator of aeration status. Soil Sci. Soc. Amer. Proc., 1975, 39(5), 870-875.
• [24] Stolzy L.H., Focht D.D. and Fluhler H.: Indicators of soil aeration. Flora, 1981, 171, 236-265.
• [25] Labuda S.Z.: Element ratios in soil on traffic circles as indices of environmental hazards. Chem. Inż. Ekol., 2005, 12(½), 93-100.
• [26] Labuda S.Z.: Trace element ratios in plants as indicators of environmental hazards. Ecol. Chem. Eng. A, 2009, 16(3), 271-276.
• [27] Labuda S.: Suppleness of soil on reduction as suggestion of a new index of soil fertility. Zesz. Probl. Post. Nauk Roln., 1995, 421a, 253-259 (in Polish).
• [28] Labuda S.: Suppleness on soil reduction as affected by soils chemical properties. Zesz. Probl. Post. Nauk Roln., 1998, 456, 83-87 (in Polish).
• [29] Labuda S.: Pliability of soil on reduction in the agronomic assessment soil properties. Proc. Sci. Conf. in the Belarusian State Agricultural Academy. Gorki, Belarus, 1999, pp. 154-157 (in Russian).
• [30] Labuda S.Z.: Soil redox potential in urban environmental studies. Proc. Sci. Conf. in the Czech University of Agriculture. Prague, Czech Republic, 2006, 137-142.
• [31] Labuda S., Mackowiak C. and Mazurkiewicz I.: Influence of organic matter and nitrogen fertlization on redox potential in the soil. Folia Univ. Agric. Stetin. 211 Agricultura, 2000, 84, 245-249 (in Polish).
• [32] Labuda S.Z., Mazurkiewicz I.. and Mackowiak C.: Redox potential in soil as affected by many years of fertilization. Chem. Inż. Ekol., 2002, 9(4), 419-429.
• [33] Labuda S.Z.: An essay on the fertilization. Ann. UMCS, Sectio E, Agricultura, 2006, 61, 1-8.
• [34] Karlen D.L., Ditzler C.A. and Andrews S.S.: Soil quality, why and how? Geoderma, 2003, 114(¾), 145-156.
• [35] Snakin V.V., Krechetov P.P. Kuzovnikova T.A., Alyabina I.O. Gurov A.F. and Stepichev A.V.: The system of assessment of soil degradation. Soil Technol., 1996, 8(4), 331-343.
• [36] Vetchnnikov A.A.: The influence of petroleum trunk-line building on dernovo-podzolic and brightly-grey forest soils. Proc. Sci. Conf. in the Nizhniy Novgorod State Agricultural Academy. Nizhniy Novgorod, Russia, 2008, 3, 10-13 (in Russian).
• [37] Vetchnnikov A.A.: The effect of liming and mineral and organic fertilizers applied on the yielding of vetch-oats intercropping with mixture mustard cultivated on the gray forest devastated soil. Plodorodie 2010, 3, 4-5 (in Russian).
• [38] Labuda S.: A new index of cation saturation state in soil. Commun. Soil Sci. Plant Anal., 1993, 24(13&14), 1603-1608.
• [39] Labuda S.: Relationship between cation saturation stage index and hydrogen ions in soil. Zesz. Probl. Post. Nauk Roln., 1994, 413, 205-207.
• [40] Covington A.K., Bates R.G. and Durst R.A.: Definition of pH scales, standard reference values, measurement of pH and related terminology. Pure & Appl. Chem., 1985, 57(3), 531-542.
• [41] Rabenhorst M.C.: Making soil oxidation-reduction potential measurements using multimeters. Soil Sci. Soc. Amer. J., 2009, 73(6), 2198-2201.