scholarly journals Nitrogen Mineralization Potential (No) in Three Kenyan Soils, Nitisols, Ferralsols and Luvisols

2018 ◽  
Vol 10 (4) ◽  
pp. 69
Author(s):  
George N. Karuku ◽  
Benson O. Mochoge
Keyword(s):  
Nitrogen Mineralization ◽  
Organic Matter Content ◽  
Field Capacity ◽  
Matter Content ◽  
Soil Types ◽  
Mineral N ◽  
Growing Period ◽  
Mineralizable N ◽  
Mineralization Potential ◽  
Potentially Mineralizable N

Nitrogen mineralization potential is important so as to prevent over-fertilization that could lead to groundwater contamination or under-fertilization that could lead to poor nutrient provision by crops leading to low yields. Three soil types were selected on the basis of groups, agro-ecological zone, organic matter content and land use. The soil samples were taken from the 0-15 and 15-30 cm depth. The samples were placed in incubation bags, water added to field capacity, sealed and incubated in laboratory at room temperature. The bags were opened at intervals of two weeks and soil sub-samples taken for analysis of mineral N for a period of 17 weeks. The calculated mineralizable N was 138.8 μg N and 116.4 μg N/g for Gituamba andosols, 46.0 μg N and 46.4 μg N/g for Kitale ferralsol and 260.1 μg N and 197.3 μg N/g soil for Katumani luvisols in the 0-15 and 15-30 cm depth, respectively. These calculated values compared well with the actual cumulative mineralizable N for Gituamba andosols at 127 μg N and 74.1 μg N/g, for Kitale ferralsols at 48.0 μg N and 64.1 μg N/g and for Katumani 80.6 μg N and 47.7 μg N/g soil in the 0-15 and 15-30 cm depth, respectively. The time taken for 50% of potentially mineralizable N to be mineralized (t½) ranged from 6.3 weeks for Katumani luvisols 15-30 cm to 30.1 weeks for Kitale ferralsols 0-15 cm soil depths. The soils with highest rate constant (k) had the least. For example, 15-30 cm depth of Katumani luvisols with of 6.3 weeks had the highest k of 0.112 week-1 compared with Kitale ferralsols 0-15 cm depth with t½ of 30.1 weeks and the lowest k of 0.023 week-1. The observed data indicates that 50% of N would be mineralized in all the soil types with the exception of Kitale ferralsols (0-15 cm depth) within the growing period of the crops which is approximately 20 weeks.

LOSS OF ORGANIC MATTER AND POTENTIALLY MINERALIZABLE NITROGEN FROM SASKATCHEWAN SOILS DUE TO CROPPING

1982 ◽  
Vol 62 (4) ◽  
pp. 651-656 ◽  
Author(s):  
C. A. CAMPBELL ◽  
W. SOUSTER
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Matter Content ◽  
Soil Medium ◽  
Organic C ◽  
Prairie Soils ◽  
Mineralizable N ◽  
Potentially Mineralizable N ◽  
Mineralizable Nitrogen ◽  
Gray Luvisol

Although it is known that considerable loss in total organic matter has occurred due to cultivation of prairie soils, there is little information on changes in the fertility-related fraction of the organic matter. Twelve prairie surface soils representing paired virgin and cultivated coarse-, medium-, and fine-textured soils from the Brown, Dark Brown, and thin Black Chernozem and Gray Luvisol soil zones were analyzed and used to assess changes in total C, N and potentially mineralizable N. Cropping caused large losses of organic C (41–53%) and N (31–56%), but losses of potentially mineralizable N (N0) were even greater for the Chernozems (55–67%) though not for the Gray Luvisols. N0 in virgin soils ranged between 133 and 401 μg N/g soil and increased from Gray Luvisol to Brown to Dark Brown to thin Black Chernozem. In cultivated soils, N0 was generally similar among soil zones and values ranged between 66 and 141 μg N/g soil. Medium-textured soils generally had the greatest organic matter content and N0. The active N fraction (N0/N) ranged between 4 and 20.5% and was greatest in Brown soils and in the coarser-textured soils. Losses of organic matter, N0, and N0/N were greatest from the coarser-textured soils. The findings of this study help to explain why a significant portion of prairie soils now require N fertilizer even after being summer-fallowed.

scholarly journals The effect of various composts on vegetable green mass on two soil types

2017 ◽  
pp. 179-183
Author(s):  
Judit Szűcsné Szolomájer ◽  
Marianna Makádi ◽  
Ibolya Demeter ◽  
Attila Tomócsik ◽  
Tibor Aranyos ◽  
...  
Keyword(s):  
Sewage Sludge ◽  
Organic Matter Content ◽  
Chemical Properties ◽  
Nutrient Content ◽  
Biological Properties ◽  
Matter Content ◽  
Soil Types ◽  
Test Plant ◽  
Positive Effects ◽  
Supply Capacity

Composting of sewage sludges makes easier the utilization of sewage sludge in the agriculture and the composts in good quality could increase the nutrient content of soil. Due to the composting process, the sewage sludge composts with high organic matter content can be utilized in the same way as other composts or farmyard manure.Composts produced in different ways have different effects on the physical, chemical and biological properties of different soils, although their positive effects have already proved in the literature. In our study the effects of composts from different composting processes were investigated in soil-plant systems. The different physical and chemical properties of the two examined soil types (arenosol and chernozem)strongly influenced the nutrient supply capacity of composts which could be characterized by the growth of ray-grass as a test plant in the pot experiment. In this work we examined the effects of three different composts on the green weight of plants on the fourth and eighth weeks after the treatment and sowing.

scholarly journals Effects on nutrient availability in agricultural soils following the application of slurry amended with additives

2021 ◽  
Author(s):  
Vito Abbruzzese
Keyword(s):  
Nutrient Availability ◽  
Agricultural Soils ◽  
Sandy Loam ◽  
Organic Matter Content ◽  
Farming Systems ◽  
Matter Content ◽  
Soil Parameters ◽  
Mineral N ◽  
Total N ◽  
Inorganic Fertiliser

In many farm systems, both inorganic and organic fertilisers, including manure and slurry, are applied to the soil to replenish nutrient offtake in agricultural products and additional nutrient losses to soil as well as surface water and groundwater. With respect to sole reliance on inorganic fertilisers, the use of manure/slurry as a nutrient resource offers important benefits, including the reuse and recycling of nitrogen (N) and phosphorus (P) within farming systems as well as a reduction in the reliance on agricultural production on finite inorganic fertiliser reserves. There is increasing interest in the extent to which additives can enhance the nutrient value of slurry/manure. However, little is known about the impacts of these amended slurries/manures on the quantity and composition of N and P within agricultural and pasture soils. We report data from incubation experiments in which soils received a range of treatments, including the application of livestock slurry that had received a mixture of commercial additives. Our experiments were designed to understand how slurry that has received additives ultimately affects nutrient availability in organic, clay-loam and sandy-loam grassland soils. The addition of the additives to slurry resulted in a slight increase or no difference in total solids, pH, total N, ammonium-N, total P, total potassium, total magnesium and total sodium compared to the untreated counterpart. We considered the effects of our treatments on a range of agronomically important soil parameters, including Olsen-P, mineral-N, available-K, pH and organic matter content. This experiment aimed to understand the extent to which soil fertility could be enhanced through the application of slurries/manures that have received additives. The application of both amended and unamended slurry treatments on soil led to higher values of NH4-N, available-K, available Mg and pH than the addition of inorganic fertiliser. In addition, no substantial differences were observed between the treatment of the three soils with unamended and amended slurry.

scholarly journals COMPARATIVE ASSESSMENT OF SOME PHYSICAL PROPERTIES AND ORGANIC MATTER CONTENT OF SOILS DERIVED FROM DIFFERENT PARENT MATERIALS IN AKWA IBOM STATE, NIGERIA

2019 ◽  
Vol 18 (1) ◽  
pp. 107-125
Author(s):  
P. C. OGUIKE ◽  
U. E. UTIN
Keyword(s):  
Organic Matter ◽  
Bulk Density ◽  
Crop Production ◽  
Alluvial Soil ◽  
Organic Matter Content ◽  
Field Capacity ◽  
Matter Content ◽  
Comparative Assessment ◽  
Parent Materials ◽  
Cumulative Infiltration

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.  

SOIL SPATIAL VARIABILITY OF SOME SOIL PROPERTIES USING FACTOR ANALYSIS IN FEDERAL COLLEGE OF FORESTRY MECHANIZATION, KADUNA RESEARCH FARM

2020 ◽  
Vol 4 (2) ◽  
pp. 695-698
Author(s):  
Akinrinshola Dare ◽  
Samson O. Okechalu ◽  
Bako Amos ◽  
Thompson Oluwole Ademola ◽  
G. Lapkat Luka
Keyword(s):  
Factor Analysis ◽  
Organic Matter ◽  
Spatial Variability ◽  
Soil Properties ◽  
Size Fraction ◽  
Organic Matter Content ◽  
Field Capacity ◽  
Sampling Procedure ◽  
Matter Content ◽  
Available Water Content

This paper shows the spatial variability of soil properties and factors that contribute to the pattern of variability in Federal College of Forestry Mechanization Research farm.   Nine (9) Soil samples were obtained from various points on the farm using random sampling procedure and these samples were subjected to further for laboratory analysis to determine the particle size fraction, soil pH, organic matter content, and from the data obtained was used to determine the Wilting Point (WP), Saturation Capacity (SC), Field Capacity (FC), Available Water Content (AW), Soil Hydraulic Conductivity (SHC), and Bulk density (BD) using SOILWAT software.  Descriptive statistics and factor analysis techniques was used to analyze the data obtained, the coefficient of variation ranged from 3.045 to 61.825% and factor analysis showed that the variability of the soil properties is as a result of the textural characteristics, and organic matter.

Nitrogen cycling in a semi-arid Mediterranean region: changes in soil N and organic matter under several crop/livestock production systems

1994 ◽  
Vol 45 (6) ◽  
pp. 1293 ◽  
Author(s):  
PF White ◽  
NK Nersoyan ◽  
S Christiansen
Keyword(s):  
Organic Matter ◽  
Organic Matter Content ◽  
Farming Systems ◽  
Matter Content ◽  
Soil N ◽  
Livestock Farming ◽  
Mineral N ◽  
North West ◽  
Total Soil ◽  
Total Soil N

There is a need to quantify the effects on soil N of introducing different legumes into the farming systems of West Asia and North Africa. This paper presents 6 years results from an on-going experiment aimed at examining the productivity of several crop/livestock farming systems in north west Syria. Changes in total soil N and organic matter when either medic pasture (3 stocking rates), vetch, lentil, fallow or watermelon were rotated yearly with wheat were examined. In addition, in the sixth year of the experiment, mineral N levels in the soil and the N content of the wheat and legumes shoots were determined in order to formulate a simple N balance for each rotation. Medic pasture and vetch rotations increased total soil N and the organic matter content of the soil. Lentil had no effect on total soil N or the organic matter content. Total soil N also remained constant in the fallow rotation, but organic matter content of the soil tended to decrease. The changes in soil properties had implications for the long term production from the different rotations, and highlighted the importance of retaining legume residues for maintaining fertility.

scholarly journals Greenhouse Gas Emissions as Affected by Fertilization Type (Pig Slurry vs. Mineral) and Soil Management in Mediterranean Rice Systems

Agronomy ◽  
2020 ◽  
Vol 10 (4) ◽  
pp. 493
Author(s):  
Beatriz Moreno-García ◽  
Mónica Guillén ◽  
Dolores Quílez
Keyword(s):  
Nitrous Oxide ◽  
Organic Matter ◽  
Greenhouse Gas ◽  
Great Increase ◽  
Ghg Emissions ◽  
Organic Matter Content ◽  
Mineral Fertilizer ◽  
Matter Content ◽  
Pig Slurry ◽  
Mineral N

The great increase in livestock production in some European areas makes it necessary to recycle organic slurries and manures and to integrate them in crop production. In Northeast Spain, the application of pig slurry (PS) is being extended to alternative crops such as rice due to the great increase in pig production. However, there is a lack of information of the effect of substitution of synthetic fertilizers with pig slurry on greenhouse gas (GHG) emissions in rice crop, and this information is key for the sustainability of these agricultural systems. The aim of this study was to evaluate the effect of the substitution of mineral fertilizers by PS on GHG emissions in Mediterranean flooded rice cultivation conditions under optimal nitrogen (N) fertilization. Two field experiments were carried out in two different (contrasting) soil types with different land management. Site 1 had been cultivated for rice in the previous three years with no puddling practices. Site 2 had been cultivated for rice for more than 15 years with puddling tillage practices and had higher organic matter content than site 1. The cumulative nitrous oxide emissions during the crop season were negative at both sites, corroborating that under flooded conditions, methane is the main contributor to global warming potential rather than nitrous oxide. The substitution of mineral fertilizer with PS before seeding at the same N rate did not increase emissions in both sites. However, at site 1 (soil with lower organic matter content), the higher PS rate applied before seeding (170 kg N ha−1) increased methane emissions compared to the treatments with lower PS rate and mineral fertilizer before seeding (120 kg N ha−1) and complemented with topdressing mineral N. Thus, a sustainable strategy for inclusion of PS in rice fertilization is the application of moderate PS rates before seeding (≈120 kg N ha−1) complemented with mineral N topdressing.

The effects of agronomy on the carbon and nitrogen contained in the soil biomass

1981 ◽  
Vol 97 (2) ◽  
pp. 319-327 ◽  
Author(s):  
T. McM. Adams ◽  
R. J. Laughlin
Keyword(s):  
Organic Matter Content ◽  
Matter Content ◽  
Arable Soils ◽  
Grassland Soils ◽  
Mineral N ◽  
Grassland Soil ◽  
Organic C ◽  
Organic Manures ◽  
Carbon And Nitrogen ◽  
Total Soil N

SummarySoils of various agronomic histories were fumigated with chloroform, and the resultant increased production of CO2 and mineral-N measured and expressed as biomass C and the flush of mineral-N production (FN), respectively. Biomass C and FN contents of grassland soils were greater than those of arable soils, and significant correlations with macro organic-matter content were found. Biomass C contents varied from 7 to mg C/100 g soil in arable soil and from 31 to 222 mg C/100 g soil in grassland or woodland. The proportion of soil organic C that was contained within the biomass ranged from 0·3 to 4·0%, whilst FN comprised from 1·0 to 11·7% of total soil N. FNcontents ranged from 1·1 to 13·2mg N/1OOg soil for arable soils, and from 2·5 to 31·7 mg N/100 g soil for grassland and woodland. Application of organic manures increased biomass C and FN contents in grassland soil.

scholarly journals Study on Soil Mobility of Two Neonicotinoid Insecticides

2016 ◽  
Vol 2016 ◽  
pp. 1-9 ◽  
Author(s):  
Mária Mörtl ◽  
Orsolya Kereki ◽  
Béla Darvas ◽  
Szandra Klátyik ◽  
Ágnes Vehovszky ◽  
...  
Keyword(s):  
Sandy Soil ◽  
Water Solubility ◽  
Binding Capacity ◽  
Organic Matter Content ◽  
High Mobility ◽  
Clay Content ◽  
Matter Content ◽  
Soil Types ◽  
Active Ingredients ◽  
Neonicotinoid Insecticide

Movement of two neonicotinoid insecticide active ingredients, clothianidin (CLO) and thiamethoxam (TMX), was investigated in different soil types (sand, clay, or loam) and in pumice. Elution profiles were determined to explore differences in binding capacity. Soil characterized by high organic matter content retained the ingredients, whereas high clay content resulted in long release of compounds. Decrease in concentration was strongly influenced by soil types: both CLO and TMX were retained in loam and clay soils and showed ready elution through sandy soil and pumice. Elution capability of the active ingredients in sandy soil correlated with their water solubility, indicating approximately 30% higher rapidity for TMX than for CLO. Soil organic carbon-water partitioning coefficients (Koc) determined were in good agreement with literature values with somewhat lower value for CLO in sandy soil and substantially higher values for TMX in clay soil. High mobility of these neonicotinoid active ingredients in given soil types urges stronger precautionary approach taken during their application.

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