Pregled bibliografske jedinice broj: 764330
The role of tillage and crops in the existence of the soil
The role of tillage and crops in the existence of the soil // Land Quality and Landscapes Processes / Tamas Herman, Gergely Toth, Tamas Kismanyoky, Attila Dunai (ur.).
Keszthely: University of Pannonia & European Commission Joint Research Centre, 2015. str. 62-69 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 764330 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
The role of tillage and crops in the existence of the soil
Autori
Kisić, Ivica ; Bogunović, Igor ; Birkas, Marta ; Jurišić, Aleksandra
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Land Quality and Landscapes Processes
/ Tamas Herman, Gergely Toth, Tamas Kismanyoky, Attila Dunai - Keszthely : University of Pannonia & European Commission Joint Research Centre, 2015, 62-69
ISBN
978-92-79-48310-3
Skup
Land Quality and Landscapes Processes
Mjesto i datum
Keszthely, Mađarska, 02.06.2015. - 04.06.2015
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
obrada tla; usjevi; gubici tla; erozija vodom
(soil tillage; crops; soil loss)
Sažetak
In order to estimate the effect of tillage and crops on water erosion soil loss was monitored on Stagnic Luvisol. The highest erosion in the 20- year investigation period was recorded in the control treatment. Following was the treatment that involved ploughing and sowing up and down the slope. Lower soil losses were recorded in no- tillage and treatments with ploughing and sowing across the slope. Higher soil losses were recorded in spring wide row crops growing (maize and soybean) comparing to the in winter crops (wheat and oilseed rape) and double crops (spring barley with soybean). In the investigation period an average loss of 0.44 cm of the plough layer was recorded in the control treatment, which means that the entire plough layer (depth 25 cm) would completely be eroded away in a period of 57 years. In ploughing and sowing up and down the slope treatment average soil loss was 0.09 cm and plough layer would completely be destroyed in a period of approximately 270 years. In all other treatments which we recommend for the area of Stagnic Luvisol the soil should be preserved for the next several thousands of years, more accurately is not endangered by erosion processes.
Izvorni jezik
Engleski
POVEZANOST RADA
Ustanove:
Agronomski fakultet, Zagreb