In the
present study, two topomorphic vertisols profiles used for sorghum production
were described and characterized. After macroscopic characterization, physicochemical,
mineralogical and geochemical analyses were made. Physicochemical analyses were
made by standard methods while mineralogy was determined on clay fraction
(˂2µm) by X-ray diffraction coupled to Fourier transform infrared spectroscopy.
Geochemical analysis was determined on 180µm fraction by inductively coupled
plasma- Atomic Emission Spectroscopy (ICP-AES) and mass spectrometry (ICP-MS).
Results revealed that studied vertisols were average deep, less differentiated
with desiccations cracks and gilgai micro relief. The angular blocky structure
and clayey texture were observed. They were alkaline (7.3 ≤ pHwater
≤ 8.4) and recorded a low to moderate organic matter and nitrogen contents.
Cation exchange capacity was high reaching 52.24 meq 100g-1 and
exchangeable cations were moderates with Ca2+ (3.69- 29.6 meq 100g-1)
the most represented cation. Vertisols were made of smectites associated to
kaolinite and a lesser content of quartz. Illites and calcite were also
identified in some horizons. On the geochemical point of view, Si02 (55.87-
83.64%), Al2O3 (6.08-20.25%), Fe2O3
(2.09-6.39%) and K2O (1.43-2.24 %) were the dominant oxides. Traces
elements were represented essentially by Ba (518-1202 mg kg-1), Zr
(334-685 mg kg-1) and Sr (71-190 mg kg-1). The overall
features are suitable to dry season sorghum production. The amount of smectites
seemed to be an important factor affecting their water holding capacity on
which dry season sorghum production depends. Improved cropping systems have to
be developed to sustain productivity in vertisols with low smectites and where
annual rainfall is lesser.
Topomorphic vertisols clay smectites dry season sorghum North Cameroon
Birincil Dil | İngilizce |
---|---|
Bölüm | Articles |
Yazarlar | |
Yayımlanma Tarihi | 1 Ekim 2018 |
Yayımlandığı Sayı | Yıl 2018 Cilt: 7 Sayı: 4 |