Description of experimental site
The study was carried out at the Department of Soil Science Teaching and Research Farm, University of Nigeria, Nsukka. The location falls within the derived savannah agro-ecological zone of Nigeria (6
o51' N, 7
o25' E) at an average elevation of about 436 m above sea level. The rainy season starts from April to October while the dry season begins from November to March. There is usually a short break in the month of August. The average annual rainfall amount is about 1600 mm and 85% of this takes place during the rainy season. The average minimum and maximum temperatures are about 22
oC and 30
oC respectively. The relative humidity was rarely below 60% (
Asadu, 2002). The soils of the area are mostly Ultisols which belongs to Nkpologu series (
Nwadialo, 1989). The soil is very deep, dark-reddish brown at the top layer and reddish in the subsoil. It is coarse to medium sandy loam (clay content ranged from 5-25%), acid in reaction (pH range of 4-7) and low in nutrient status.
Experimental layout
The experiment was first carried out in the greenhouse and later evaluated in the field. The greenhouse experiment was laid out in a completely randomized design (CRD), while the field experiment was laid out in a randomized complete block design (RCBD). The treatments applied were poultry manure (PM) and pig slurry (PS) at 10, 20 and 40 t ha
-1 respectively, NPK 15:15:15 at 300 kg/ha and control with no amendment.
Greenhouse study
The soil used for the greenhouse study was collected from the Teaching and Research Farm of the Department of Soil Science, University of Nigeria, Nsukka. Air-dried sieved (2 mm) soil (3.5 kg) was placed in each perforated pots following CRD with eight (8) treatments replicated five times. Poultry manure and pig slurry were added at 10, 20 and 40 t ha
-1. All the pots were watered to field capacity for two weeks (3 times per week). At the end of two weeks, the okra (Spineless species) seeds were planted at the rate of two seeds per pot. The germinated seedlings were thinned down to one per pot two weeks after planting (WAP). The recommended rate of NPK 15-15-15 fertilizer (300 kg ha
-1) was applied two weeks after planting (WAP) to five pots while the remaining five pots with no amendment served as the control. The okra plants were harvested at eight WAP.
Field study
The field evaluation was carried out from 10
th April, 2018 to 15
th July, 2018 at the Teaching and Research Farm of the Department of Soil Science, University of Nigeria, Nsukka. Each of the plots (3 m × 1.5 m) were properly demarcated using earthen bunds with a spacing of 0.5 m between each plot and a spacing of 1 m between each blocks. There were 40 experimental plots under randomized complete block design (RCBD) with five replications. The plots were manually tilled to 20 cm depth using hand hoe. The poultry manure and pig slurry at 10, 20 and 40 t ha
-1 were thoroughly mixed in plots as per treatments before planting. The okra (Spinelees species) seeds were planted at the rate of two seeds per hole using a plant spacing of 60 cm × 50 cm and thinned to one, two weeks after planting. The recommended NPK 15-15-15 fertilizer (300 kg/ha) was applied two weeks after planting to five plots while the remaining five plots without any amendment served as control. Weeding was done by hand and hand hoe picking. Subsequent weed controls were done by a combination of hand picking and use of hand hoe method at two weeks interval.
Data collection and soil sampling
The agronomic parameters such as plant height and number of leaves were measured at 2, 4, 6 and 8 weeks after planting (WAP) in greenhouse and field studies. Fresh and dry matter yields were also measured. Both disturbed and undisturbed soil samples were collected at 0-15 cm depth with the help of core samplers and soil auger. The soil samples were collected in black polyethylene bags. The disturbed soil samples were air dried, sieved with 2 mm sieve while the core samples were trimmed with spatula and saturated for at least 48 hours before analysis. The soil analysis were done using standard laboratory procedures.
Laboratory analysis
Particle size distribution of the soil was determined using the Bouyoucous hydrometer method as described by
Gee and Bauder (1986). Bulk density was determined by core method as described by
Blake and Hartge (1986).
Saturated hydraulic conductivity (Ksat) was determined by the constant head permeameter method (
Klute and Dirksen, 1986). Darcy’s equation for analysis of constant head method, as described by
Youngs (2001) was used for the computation of Ksat as follows:
…… (1)
Where
Q is steady state volume of outflow from the entire soil column (cm
3), L is the length of soil column (cm), A is the interior cross-sectional area of the soil column (cm
2), T is the time of flow (sec), ΔH is the change in hydraulic head or the head pressure difference causing the flow (cm).
Total porosity (P) was computed from bulk density (Bd), using the equation below (assumed particle density p
s = 2.65 Mg m
-3):
…….. (2)
The size distribution of water stable aggregates (WSA) was determined by the wet sieving method (
Kemper and Rosenau, 1986). In this method, 25 g of the air-dried soil sample retained on 2 mm sieve was weighed out and put on the topmost of the nest of sieves of 2, 1, 0.5 and 0.25 mm. The content was soaked initially for 5 minutes to prevent slaking and thereafter oscillated vertically in water for 5 min at the rate of 30 oscillations per minute and at an amplitude of 4 cm. Thereafter, soil aggregates left on each sieve were oven dried at 105
oC for 24 hours and weighed. The aggregate stability (AS) as percent of water-stable aggregates (WSA) > 0.5 mm on each sieve were determined thus:
........ (3)
Where
Mwsa = Mass of water stable aggregates > 0.5 mm plus sand (g).
Ms = Mass of the sand fraction alone (g).
Mt = Total mass of the sieved soil (g).
The MWD of WSA was calculated based on the equation proposed by
Chaney and Swift (1984) as:
...…. (4)
Where
x
i = The mean diameter of any particular size range of aggregates separated by sieving and w
i = The weight of aggregates in that size range as a fraction of the total initial dry weight (25 g) of soil used.
Soil pH was determined using digital pH meter in a soil solution ration of 1:2.5. Organic carbon was determined using the modified Walkley and Black method as described by
Nelson and Sommer (1996). The soil organic matter was obtained by multiplying with a correction factor of 1.724. Total nitrogen was determined using the Kjeldhal method as described by
Bremner (1996). Available phosphorus was determined using Bray II method as described by
Bray and Kurtz (1945). Exchangeable calcium, magnesium, sodium and potassium were extracted with NH4OAc. Calcium and magnesium were determined using Ethylene Diamine Tetra-acetic acid (EDTA) titration method while potassium and sodium were determined using flame photometer. Cation exchange capacity was determined titrimetrically using 0.01N NaOH. Exchangeable acidity was determined titrimetrically using 0.05 N NaOH.
Data analysis
The soil and agronomic data were analyzed for variance (ANOVA) in RCBD and in CRD for the field and the greenhouse study as outlined by
Steel and Torrie (1980) using GENSTAT 4.0. Separation of treatment means was done using the F-LSD at 5% probability level as described by
Obi (2002).