Pregled bibliografske jedinice broj: 437393
Geochemical background in soils : a linear process domain? An example from Istria (Croatia)
Geochemical background in soils : a linear process domain? An example from Istria (Croatia) // Environmental Earth Sciences, 59 (2010), 6; 1367-1383 doi:10.1007/s12665-009-0125-2 (međunarodna recenzija, članak, znanstveni)
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Naslov
Geochemical background in soils : a linear process domain? An example from Istria (Croatia)
Autori
Peh, Zoran ; Miko, Slobodan ; Hasan, Ozren
Izvornik
Environmental Earth Sciences (1866-6280) 59
(2010), 6;
1367-1383
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
soil-forming processes; non-linear dynamics; geochemical background; normal distribution; dissipative structures; Istria; Croatia
Sažetak
Definition of geochemical background in exploration and environmental geochemistry has always been regarded as contingent upon scale and investigated locality but mostly under assumption that hosts of processes that produce the data more or less conform individually to Gaussian law of "central tendencies". Recently, understanding of pedogenesis as synergetic process being characterized by non-linear dynamics renders thermodynamic approach directly applicable in assessment of geochemical thresholds, with concepts of linearity and normality set alongside in solving the problems of soil geochemistry. Seen from this perspective the work is an attempt to relate conceptual fundamentals of non-linear dynamical theory to basic statistical methods in order to elucidate the nature and origins of element subpopulations hidden in the original geochemical data from the soils of Istrian Peninsula (western Croatia). To this purpose the two major groups of soils were selected for analysis depending on the type of bedrock as one of the main soil-forming factors. Geochemical data were subjected to the trimming procedure by which the outliers were removed from the total data collective and attributed to non-linear causes precluding simple cause-and-effect relationships as the sine qua non of Gaussian distribution. Geochemical background is then defined as the normal range of data of the remaining (trimmed) dataset indicating the "thermodynamic branch" of the specific soil processes as opposed to outliers being described as dissipative structures.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
181-1811096-1104 - Karta mineralnih sirovina Republike Hrvatske (Peh, Zoran, MZOS ) ( CroRIS)
181-1811096-1181 - Osnovna geokemijska karta Republike Hrvatske (Halamić, Josip, MZOS ) ( CroRIS)
181-1953068-0363 - Holocenski sedimenti kao zapis promjena u okolišu Jadranskih slivova (Koch, Georg, MZOS ) ( CroRIS)
Ustanove:
Hrvatski geološki institut
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus