Pregled bibliografske jedinice broj: 855044
Spatial variability of total carbon and soil organic carbon in agricultural soils in Baranja region, Croatia
Spatial variability of total carbon and soil organic carbon in agricultural soils in Baranja region, Croatia // Geophysical Research Abstracts Vol. 19, EGU2017-703, 2017 EGU General Assembly 2017
Beč: European Geosciences Union (EGU), 2017. str. 703-703 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 855044 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Spatial variability of total carbon and soil organic carbon in agricultural soils in Baranja region, Croatia
Autori
Igor, Bogunović ; Sebastiano, Trevisani ; Paulo, Pereira ; Miranda, Šeput
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Geophysical Research Abstracts Vol. 19, EGU2017-703, 2017 EGU General Assembly 2017
/ - Beč : European Geosciences Union (EGU), 2017, 703-703
Skup
European Geosciences Union General Assembly 2017
Mjesto i datum
Beč, Austrija, 23.04.2017. - 28.04.2017
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Climate change; agroecosystem; GIS; prediction
Sažetak
Climate change is expected to have an important influence on the crop production in agricultural regions. Soil carbon represents an important soil property that contributes to mitigate the negative influence of climate change on intensive cropped areas. Based on 5063 soil samples sampled from soil top layer (0-30 cm) we studied the spatial distribution of total carbon (TC) and soil organic carbon (SOC) content in various soil types Anthrosols, Cambisols, Chernozems, Fluvisols, Gleysols, Luvisols) in Baranja region, Croatia. TC concentrations ranged from 2.10 to 66.15 mg/kg (with a mean of 16.31 mg/kg). SOC concentrations ranged from 1.86 to 58.00 mg/kg (with a mean of 13.35 mg/kg). TC and SOC showed moderate heterogeneity with coefficient of variation (CV) of 51.3% and 33.8%, respectively. Average concentrations of soil TC vary in function of soil types in the following decreasing order: Anthrosols (20.9 mg/kg) > Gleysols (19.3 mg/kg) > Fluvisols (15.6 mg/kg) > Chernozems (14.2 mg/kg) > Luvisols (12.6 mg/kg) > Cambisols (11.1 mg/kg), while SOC concentrations follow next order: Gleysols (15.4 mg/kg) > Fluvisols (13.2 mg/kg) = Anthrosols (13.2 mg/kg) > Chernozems (12.6 mg/kg) > Luvisols (11.4 mg/kg) > Cambisols (10.5 mg/kg). Performed geostatistical analysis of TC and SOC ; both the experimental variograms as well as the interpolated maps reveal quite different spatial patterns of the two studied soil properties. The analysis of the spatial variability and of the spatial patterns of the produced maps show that SOC is likely influenced by antrophic processes. Spatial variability of SOC indicates soil health deterioration on an important significant portion of the studied area ; this suggests the need for future adoption of environmentally friendly soil management in the Baranja region. Regional maps of TC and SOC provide quantitative information for regional planning and environmental monitoring and protection purposes.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Poljoprivreda (agronomija)