Physical and chemical characterization of some selected soils in University of Maiduguri, Borno State Nigeria

2021 ◽  
pp. 32-41
Author(s):  
Buji I.B. ◽  
Adamu I. ◽  
Magaji M.J. ◽  
Hayatu N.G. ◽  
Zubairu A.M. ◽  
...  

A semi-detailed survey was conducted to characterize some physical and chemical properties of soils of Teaching and Research Farm University of Maiduguri, Borno State. Three sites were selected on the basis of land forms and surface texture and their description were taken using two soil profile pits at each sites. The soils collected were subjected to laboratory analysis using standard procedure. The colour of the soils changes at both surface and subsurface layers within each layer due to reduction in organic matter content down the profile, majority of the topsoil layer were brown while light yellowish orange were found in the subsoil layer.The consistency of the soil changed from hard at the surface layers to soft at subsurface layers. Soil reaction ranged from6.72 to 7.36which is neutral to slightly alkaline at both surface and subsurface layer and the electrical conductivity shows no salinity effect at both surface and subsurface layers. Cation Exchange Capacacity ranged from 10.09 to 15.97 Cmol/kg which was very low. Organic carbon content was generally low to moderate which ranged from 0.2 to 0.60 % due to poor return in organic matter content. The soil texture of the surface and subsurface was predominately sandy loam. Sand content of P2 ranged from 537g/kg to 762 g/kg, silt ranged from 141 (P4) to 441 (P1) g/kg and clay from 72 (P2) and 147 (P4) g/kg. Available phosphorus and potassium tend to be low while sodium was high, magnesium showed to be medium to high, while calcium was also low to medium. Bulk density of the soils, increases with increase in depth and the hydraulic conductivity decreases with increase in depth. The chemical and physical properties of the soil are good for crop production except for sodium that is high, which need some management practices for optimum crop production and as such evaluation on the capability and suitability of the area should be conducted.

Author(s):  
Amita M Watkar ◽  

Soil, itself means Soul of Infinite Life. Soil is the naturally occurring unconsolidated or loose covering on the earth’s surface. Physical properties depend upon the amount, size, shape, arrangement, and mineral composition of soil particles. It also depends on the organic matter content and pore spaces. Chemical properties depend on the Inorganic and organic matter present in the soil. Soils are the essential components of the environment and foundation resources for nearly all types of land use, besides being the most important component of sustainable agriculture. Therefore, assessment of soil quality and its direction of change with time is an ideal and primary indicator of sustainable agricultural land management. Soil quality indicators refer to measurable soil attributes that influence the capacity of a soil to function, within the limits imposed by the ecosystem, to preserve biological productivity and environmental quality and promote plant, animal and human health. The present study is to assess these soil attributes such as physical and chemical properties season-wise.


Author(s):  
Juliana Vantellingen ◽  
Sean C. Thomas

Log landings are areas within managed forests used to process and store felled trees prior to transport. Through their construction and use soil is removed or redistributed, compacted, and organic matter contents may be increased by incorporation of wood fragments. The effects of these changes to soil properties on methane (CH<sub>4</sub>) flux is unclear and unstudied. We quantified CH<sub>4</sub> flux rates from year-old landings in Ontario, Canada, and examined spatial variability and relationships to soil properties within these sites. Landings emitted CH<sub>4</sub> throughout the growing season; the average CH<sub>4</sub> emission rate from log landings was 69.2 ± 12.8 nmol m<sup>-2</sup> s<sup>-1</sup> (26.2 ± 4.8 g CH<sub>4</sub> C m<sup>-2</sup> y<sup>-1</sup>), a rate comparable to CH<sub>4</sub>-emitting wetlands. Emission rates were correlated to soil pH, organic matter content and quantities of buried woody debris. These properties led to strong CH<sub>4</sub> emissions, or “hotspots”, in certain areas of landings, particularly where processing of logs occurred and incorporated woody debris into the soil. At the forest level, emissions from landings were estimated to offset ~12% of CH<sub>4</sub> consumption from soils within the harvest area, although making up only ~0.5% of the harvest area. Management practices to avoid or remediate these emissions should be developed as a priority measure in “climate-smart” forestry.


2018 ◽  
Vol 13 (No. 3) ◽  
pp. 140-149 ◽  
Author(s):  
Šimanský Vladimír ◽  
Lukáč Martin

Soil structure is a key determinant of many soil environmental processes and is essential for supporting terrestrial ecosystem productivity. Management of arable soils plays a significant role in forming and maintaining their structure. Between 1994 and 2011, we studied the influence of soil tillage and fertilisation regimes on the stability of soil structure of loamy Haplic Luvisol in a replicated long-term field experiment in the Dolná Malanta locality (Slovakia). Soil samples were repeatedly collected from plots exposed to the following treatments: conventional tillage (CT) and minimum tillage (MT) combined with conventional (NPK) and crop residue-enhanced fertilisation (CR+NPK). MT resulted in an increase of critical soil organic matter content (St) by 7% in comparison with CT. Addition of crop residues and NPK fertilisers significantly increased St values (by 7%) in comparison with NPK-only treatments. Soil tillage and fertilisation did not have any significant impact on other parameters of soil structure such as dry sieving mean weight diameters (MWD), mean weight diameter of water-stable aggregates (MWD<sub>WSA</sub>), vulnerability coefficient (Kv), stability index of water-stable aggregates (Sw), index of crusting (Ic), contents of water-stable macro- (WSA<sub>ma</sub>) and micro-aggregates (WSA<sub>mi</sub>). Ic was correlated with organic matter content in all combinations of treatments. Surprisingly, humus quality did not interact with soil management practices to affect soil structure parameters. Higher sums of base cations, CEC and base saturation (Bs) were linked to higher Sw values, however higher values of hydrolytic acidity (Ha) resulted in lower aggregate stability in CT treatments. Higher content of K<sup>+</sup> was responsible for higher values of MWD<sub>WSA </sub>and MWD in CT. In MT, contents of Ca<sup>2+</sup>, Mg<sup>2+ </sup>and Na<sup>+</sup> were significantly correlated with contents of WSA<sub>mi </sub>and WSA<sub>ma</sub>. Higher contents of Na<sup>+</sup> negatively affected St values and positive correlations were detected between Ca<sup>2+</sup>, Mg<sup>2+ </sup>and Na<sup>+</sup> and Ic in NPK treatments.


Soil Research ◽  
1980 ◽  
Vol 18 (2) ◽  
pp. 163 ◽  
Author(s):  
EL Greacen ◽  
R Sands

The problem of soil compaction in forestry differs from that in agriculture because of differences in the nature of the crop, in particular the weight and size of the plant members and the length of time that they persist. The roots compact the soil as they increase in size, but they also transmit the weight of the tree and forces generated by the wind onto the soil. There are important differences in management practices; in forestry modern harvesting machines apply heavy loads and, for reasons of cost, tend to be kept in operation throughout the year. As a consequence the structure of the soil suffers some damage, often manifested as compaction. Compaction arising from such sources may reduce the growth of the current trees or trees subsequently planted on the site. But it is difficult to predict the extent of such reduction, if any, because of the complex of interactions involved. Important factors concerned, namely, the soil water regime and the organic matter content, are emphasized. A conceptual model is proposed as a predictive tool. The mechanics of soil compaction, the effects of compaction on the physical properties of the soil, and techniques for the prevention and amelioration of compaction of forest soils, are discussed.


2006 ◽  
Vol 63 (2) ◽  
pp. 187-193 ◽  
Author(s):  
Marcos Gervasio Pereira ◽  
Gustavo Souza Valladares ◽  
Lúcia Helena Cunha dos Anjos ◽  
Vinícius de Melo Benites ◽  
Ademar Espíndula Jr. ◽  
...  

Soil taxonomy systems distinguish mineral soils from organic soils based on the amount of soil organic carbon. Procedures adopted in soil surveys for organic carbon measurement are therefore of major importance to classify the soils, and to correlate their properties with data from other studies. To evaluate different methods for measuring organic carbon and organic matter content in Histosols and soils with histic horizons, from different regions of Brazil, 53 soil samples were comparatively analyzed by the methods of Walkley & Black (modified), Embrapa, Yeomans & Bremner, modified Yeomans & Bremner, muffle furnace, and CHN. The modified Walkley & Black (C-W & B md) and the combustion of organic matter in the muffle furnace (OM-Muffle) were the most suitable for the samples with high organic carbon content. Based on regression analysis data, the OM-muffle may be estimated from C-W & B md by applying a factor that ranges from 2.00 to 2.19 with 95% of probability. The factor 2.10, the average value, is suggested to convert results obtained by these methods.


2018 ◽  
Vol 189 (2) ◽  
pp. 9 ◽  
Author(s):  
Maxime Debret ◽  
Yoann Copard ◽  
Antonin Van Exem ◽  
Geneviève Bessereau ◽  
Frank Haeseler ◽  
...  

Organic matter studies find an echo within different topics such as biogeochemical cycles, processes occurring in continental surfaces, anthropogenic activities, climate science, earth and planetary sciences, etc. Today’s challenges include finding and developing the most appropriate method(s) supporting the differentiation and characterisation of various types of recalcitrant organic matter in modern environments. In this study, we focus on combustion residues and coals as these two types of organic matter contain a significant amount of so-called recalcitrant organic carbon (black carbon and fossil organic carbon). Both these materials are ubiquitous, broadly stem from the same living organisms and have similar polyaromatic structures. In this respect, we tested a spectrophotometry method, classically used for sedimentology, as a very fast method for preliminary investigations. Analyses were performed with a wide range of standards and referenced samples. The results discriminate three different spectral signatures related to the degree of transformation of organic matter related to the degree of aromaticity (i.e. carbonisation). Using calibration curves, total organic carbon content can be estimated in experimental mixes with mineral matter and in a real context using subsurface sample (Gironville 101 borehole, Paris Basin, France). This method has particularly high sensitivity to very low organic matter content and is shown to be promising for a rapid evaluation of the organic carbon content.


2019 ◽  
Vol 18 (1) ◽  
pp. 107-125
Author(s):  
P. C. OGUIKE ◽  
U. E. UTIN

The study of soils derived from different parent materials is useful in formulating appropriate management schemes for soil health and agricultural production. A comparative assessment of some physical properties and organic matter content of soils formed from coastal plain sands (CPS), sandstone (SST) and river alluvium (ALV) was conducted in Akwa Ibom State, Nigeria. Topsoil samples (0 – 30 cm) were collected from ten points in soils of each of the three parent materials for laboratory analyses. The soil samples were analyzed for texture, macro and micro aggregate stability indices, soil water characteristics, bulk density and organic matter. Data generated were subjected to Analysis of Variance to compare properties of soils of the different parent materials. Significantly different means were separated using the Least Significant Difference at 5% probability level. Results showed that soils of SST and CPS parent materials both had loamy sand texture while that of ALV soil was clay. Bulk density of ALV soil (1.20 Mg m-3) was significantly lower (p≤0.05) than those of CPS (1.55 Mg m-3) and SST (1.39 Mg m-3).  Significantly higher (p≤0.05) mean weight diameter (MWD) (2.01 mm), aggregated silt+clay (51.96%) and clay flocculation index (89.00%) were observed in ALV soils than in CPS and SST soils while the dispersion ratio and clay dispersion index were significantly higher (p≤0.05) in CPS and SST soils than in the ALV soil. Alluvial soil had significantly higher (p≤0.05) saturation water content (SWC), field capacity (FC), permanent wilting point (PWP) and available water content (AWC) of 0.61, 0.45, 0.25 and 0.20 m3 m-3, respectively, than those of CPS and SST. Alluvial soil also had the lowest cumulative infiltration (3.05 cm) and saturated hydraulic conductivity (0.40 cm hr-1) relative to those of CPS and SST. The CPS soil had significantly lower (p≤0.05) organic matter content (2.07%) than SST (3.06%) and ALV (3.34%) soils. Cumulative infiltration (I) significantly and positively correlated with total sand (TS) (r = 0.710*) in the CPS soil, and Ksat (r = 0.681*), MWD (r = 0.829**) and CFI (r = 0.655*) in the SST soil. In the ALV soil, cumulative infiltration positively correlated with total porosity (r = 0.770**) and negatively with bulk density (r = - 0.770**). Saturated hydraulic conductivity (Ksat) had a positive correlation with SWC (r = 0.745*) and TP (r = 0.833**), but a significant and negative correlation with BD (r = - 0.833**) in SST soil. Field capacity (FC) positively and significantly correlated with TP (r = 0.638*) in CPS soil, and with MWD (r = 0.713*), CFI (r = 0.647*) and OM (r = 0.651*) in SST soil and with TP (r = 0.790**) and OM (r = 0.672*) in ALV soil. The correlations of FC with BD (r = - 0.638*) in CPS soil, with CDI (r = -0.647*) in SST soil and with BD (r = -0.790**) in ALV soil were significant and negative. MWD positively and significantly correlated with organic matter (r = 0.699*).  The clayey ALV soil will be suitable for paddy rice production and dry season crops due to its higher water retention capacity than the CPS and SST soils which will be better utilized for vegetable crop production under irrigation. The CPS and SST soils can also be applied to intensive crop production under rain fed condition and supplemented with irrigation.  


Author(s):  
Job Teixeira de Oliveira ◽  
Cassiano Garcia Roque ◽  
Rubens Alves de Oliveira ◽  
Rafael Montanari ◽  
Claudinei Martins Guimarães ◽  
...  

The common bean (Phaseolus vulgaris L) can be cultivated practically throughout the year in different regions of Brazil, provided there are no water and temperature limitations. This study was carried out in a Quartzarenic Neosol, in the municipality of Cassilândia, state of Mato Grosso do Sul (MS), Brazil, in the 2016/2017 agricultural year. This study aimed to establish the linear and spatial interrelations of the penetration resistance (PR), gravimetric moisture (GM), and organic matter content (OM) with bean grain yield (GY) in the 0.00-0.10 and 0.10-0.20 m soil layers, collected in a mesh of 117 georeferenced points [81 points of the base mesh (6 m spacing among points)] and 36 mesh points with higher density (2 m spacing among points). Data analysis was carried out by statistical and geostatistical techniques that enabled to note that the organic matter content correlates linearly and negatively with penetration resistance, indicating that soil management practices aiming to increase its profile improve its physical conditions and therefore the bean grain development and yield. The gravimetric moisture and soil organic matter content correlate spatially, directly, and linearly with bean grain yield, proving to be the best properties among those surveyed to estimate and increase its agricultural productivity.


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