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Both types of soil are suitable for agriculture, but, because of the slow rate of biological activity in the northern climate, they require heavy fertilization.
Both types of soil also contain illite and kaolinite, which are each concentrated in the upper horizons of the soils and are considered to be detrital.
Due to similarity in behaviour of lime treated soils and naturally structured soils, the formulation can be applied to both types of soil.
Adding CR particles by reducing the aggregate fractal dimension, soil penetration resistance and bulk density, improves soil structure in both types of soil.
Based on the data presented in this table, it becomes clear that increasing different amounts of CR has not significantly affected the EC and pH of both types of soil in this limited period of incubation.
The trend due to 0.6 g intensity level was different from that of 0.3 g intensity due to the yielding of the shear keys during the larger intensity motions for both types of soil.
Similar(54)
The results show that, for both types of soils used in this study and for the two discharge rates, the vertical component of the wetting front was greater for the pulse than for the continuous irrigation for a time equal to irrigation duration.
This research revealed that the addition of CR significantly decreased soil penetration resistance in both types of soils.
pH changes were quite different in both types of soils so that, by increasing the amount of crumb rubber, loamy sand soil's pH value decreases, whereas silty clay soil's pH was increased.
By studying the soil moisture characteristic curve at the difference treatment levels (0.12, 0.24, 0.36 and 0.48 g of crumb rubber/kg soil), it was revealed that by addition of CR application rate, water content increased at each suction point in both types of soils and maximum water content was gained at highest application rate of CR (0.48 g kg−1) (Fig. 1).
The incorporation of both types of organic matter improved soil quality (i.e., higher pH, more C and nutrients) and led to the recovery of vegetation growth (i.e., development of seedlings and higher above- and belowground biomass).
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