Effect Of Tillage On Carbon And Nitrogen Sequestration In Soils

dc.Degree M.Sc en_US
dc.Faculty Agriculture en_US
dc.contributor.advisor Omer Mohamed Eltom en_US
dc.contributor.author Ibrahim, Ibrahim Abdaldaim
dc.contributor.faculty Agricultural Engineering en_US
dc.date.accessioned 2015-05-13T10:02:43Z
dc.date.available 2015-05-13T10:02:43Z
dc.date.issued 2015-05-13
dc.date.submitted 2015-05-13
dc.description September 2004 en_US
dc.description.abstract Loss of soil organic matter (SOM) has been associated with increased tillage intensity. To investigate the effect of tillage on soil organic carbon (O.C) and total nitrogen (T.N) sequestration and hydraulic conductivity (H.C) two sites were selected for this study, the first site (Elselete North) was conventionally cultivated (sub- soiler, smoothing by disk harrow, leveling and ridging) and was compared with grassland (G.L) (control). The second site (Elgrouf Shambat) was traditionally cultivated (plough drawn by animal) and similarly compared with grassland (G.L) (control). Soil samples were taken from profiles at an interval of 7.5 cm to a depth of 30 cm. Across all soil depths, content O.C reported in traditional tillage (T.T) were significantly (P X04; 0.017 – 0.004) higher than that of conventional tillage (C.T), while tillage showed no significant differences in T.N content. In the 0 – 7.5cm soil depth, tillage had no effect on T.N and H.C, while O.C determined in T.T (14.82 gkg-1) was significantly (P X04; 0.017) higher than that of C.T (9.26 gkg-1). In the 7.5-15 cm depth, H.C in T.T (0.250cm/min) was significantly (P X04;0.05) higher than that of C.T (0.038 cm/min). In this depth (7.5-15cm), O.C in T.T (14.56 gkg-1) was significantly (P X04; 0.05) higher than that of C.T (8.58 gkg-1). In the third depth (15-22.5cm), O.C in T.T (15.08 gkg-1) was significantly (P X04; 0.01) higher than that of C.T (7.28 gkg-1), and in the same depth T.N in G.L (0.37 gkg-1) was significantly (P X04; 0.05) higher than that of C.T (0.19 gkg-1). In the lower soil depth (22.5-30cm), O.C in T.T (14.82 gkg-1) was significantly (P X04; 0.004) higher than that of C.T (7.89 gkg-1), and in the same depth O.C in G.L (16.9 gkg-1) was significantly (P X04; 0.05) higher than that of T.T (14.82 gkg-1), similarly, T.N in the T.T (0.42 gkg-1) was significantly (P X04; 0.05) higher than that of G.L (0.23 gkg-1). H.C in the G.L (0.068cm/min) was significantly (P X04; 0.05) higher than that of C.T (0.016cm/min). Modeling O.C of C.T and T.T showed that it was best fitted to the exponential model ( R2 = 40%), while T.N was best fitted to the logarithmic model (R2 = 89%) followed by the liner model (R2 = 84%). en_US
dc.description.sponsorship UOFK en_US
dc.identifier.uri http://khartoumspace.uofk.edu/handle/123456789/10707
dc.publisher UOFK en_US
dc.subject Tillage,Carbon,Nitrogen,Soils en_US
dc.title Effect Of Tillage On Carbon And Nitrogen Sequestration In Soils en_US
dc.type Thesis en_US
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