dc.description.abstract |
Knowledge of the kinds and properties of soils is critical for making decisions for crop
production and land use types. This study was conducted to determine the physic-chemical
properties and identify the major soils of the Chimchimit micro-watershed in West of Mount
Guna, South Gondar Zone, Northwest Ethiopia. A reconnaissance survey with extensive
visual observations and descriptions was conducted. The micro-watershed was classified into
upper, middle, and lower slope positions. A total of 15 disturbed soil samples and 15
undisturbed soil samples were collected from the six profiles to characterize and classify the
soils. Based on the results, the colour of the surface soils varied from yellowish brown (10YR
4/2) when dry to dark brown (10YR 3/3) when moist condition. The soil consistencies at the
surface profiles were soft to very hard (when dry) and slightly sticky to sticky, non-plastic to
plastic when (wet). The soil structure was wedge-shaped and lumpy, angular blocky to sub
angular and granular to prismatic in surface soil. The textural classes of all profiles varied
from loam to heavy clay. The bulk density of the surface horizon was lower than that of the
subsurface horizons. The total porosity increases as the bulk density decreases and vice versa.
The soil water at FC, PWP, and AWC increased with clay content and with depth. The soil
pH value varied from 4.92 at the surface to 6.5 at the subsurface horizon and rated as strongly
acidic to slightly acidic. The exchangeable (Ca
2+
& Mg
2+
),CEC and PBS were rated as
medium to very high. Whereas ex. K,
+
varied from very low to very high and ex. Na
was
rated as low. The TN and OM content of the surface layers were rated as low to high. The Av.
P content was belonging with low rate. The extractable Fe,Mn,Cu and Zn were rated as high,
medium to high, low to medium and low to high respectively at all profiles. Based on the
morphological and physicochemical properties and results, the soils of study area were
classified as Eutric Cambisols, Leptic Regosols, Dystric Cambisols and Chromic Luvisols.
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