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Roy, et al.

                water infiltration and storage, irrigation and drainage,   department’s experimental field (22°27’58” N 91°46’49”
                nutrient  and  pollutant  leaching,  runoff  and  catchment   E) of the Chittagong University. Samples of soil were
                management, and the potentiality of soils with regard   taken between 0 and 15 cm below the surface. Following
                to productivity  all depend on the saturated  hydraulic   collection, samples were broken through gentle crushing
                conductivity (Ks) of the soil. 2,14,15  The Ks is influenced by   with a wooden hammer and allowed to air dry.  The
                soil properties, soil depth, vegetation types, management   samples of soil were then passed through a 2  mm
                practices,  and so on. 16-19  Among the physical indices,   stainless steel sieve. The sieved samples were kept for
                the  saturated  Ks  change  with  soil  texture,  geometry   the purpose of analyzing the soil’s chemical and physical
                of  soil  particles,  porosity,  and  bulk  density. 20,21   It  is   characteristics. 25,26   Bulk  vermicompost  was  collected
                noteworthy that different management approaches and   from an organic farm, air-dried, and sieved to separate
                the  incorporation  of  organic  amendments  have  been   into different size fractions, namely, raw, 1.0 – 2.0 mm,
                shown to affect the saturated Ks of soils. 2,22,23  However,   0.5 – 1.0 mm, and <0.5 mm. Figure 1 shows different
                the saturated hydraulic conductivity and other hydraulic   size fractions of vermicast used for this experiment.
                properties of soils seem to be significantly impacted by   To set up the experiment, 100 g (on oven dry weight
                the  variability  of particle  size  distributions.  Both the   basis) of 2 mm sieved soil samples were weighed. Then,
                distribution of soil particle sizes or soil texture and the   the required amount of vermicast of different size ranges
                spatial arrangement of these particles or soil structure   for the rates of 5 t/ha, 10 t/ha, 15 t/ha, and 20 t/ha were
                affect the Ks values. 24                            weighed and thoroughly mixed with the previously
                  At present, there is a paucity of knowledge regarding   weighed soil samples. The incorporation of vermicast
                the link between vermicast size and Ks. Although the   resulted in five different treatments for each soil type.
                effects of soil texture and types of organic manure on   The treatment arrangement comprising different sizes of
                Ks of soils have been studied separately, to the best of   vermicast is shown in Table 1. For every experimental
                the author’s knowledge, none of the previous research   condition, we compared the results and treatments with
                manifests the effects of vermicast size on the Ks, and   a control setup and performed a reasonable number of
                how cast sizes affect conductivity in different textural   replications (Table 1).
                classes of soils. Therefore, this study investigates the   After mixing up the soil and vermicast of different
                impact of adding different size fractions of vermicast on   sizes independently, the samples were packed in the
                the Ks of two distinct soil types and clearly illustrates   aluminum core (4 cm in height and 5.6 cm in diameter),
                how  the  various  vermicast  sizes  affect  the  saturated   maintaining a roughly uniform bulk density. Amended
                hydraulic conductivity.                             and controlled soils inside  the  cores were initially
                                                                    subjected to wetting from the bottom. After complete
                2. Materials and methods                            saturation, distilled water was passed through the soil-
                                                                    filled cores. By maintaining a constant water load, the
                The soil samples for this investigation were collected   Ks were determined by measuring the volume of water
                from two distinct, undisturbed locations on the campus   passing through the soil column. The amount of water
                of Chittagong University that differed widely in terms   passed  through  the  soil  column  was measured  using
                of  soil  texture.  From  the  field  next  to  Ansar  camp   a measuring  cylinder, and the  data  were recorded  to
                (22°27’56” N 91°46’46” E), loamy soil was collected,   calculate Ks.  The Ks of both soils was calculated using
                                                                               25
                and sandy loam soil was taken from the soil science   the following formula:
















                                             Figure 1. Different size fractions of vermicast



                Volume 22 Issue 1 (2025)                       116                                 doi: 10.36922/ajwep.7526
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