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Physical Properties, Potentials And Vulnerability Of The Soils Of Sombreiro Warri Deltaic Plain, Nigeria

Kamalu O. J1. and Orji O. A.2

1Crop and Soil Science Department, University of Port Harcourt, Port Harcourt P.M.B.5323 Port Harcourt

2Crop/Soil Science Department, Rivers State University Nkpolu-Oruworukwo, Port Harcourt

IOSR Journal of Agriculture and Veterinary Science (IOSR-JAVS) e-ISSN: 2319-2380, p-ISSN: 2319-2372. Volume 11, Issue 3 Ver. II (March 2018), PP 01-11

Abstract:

This paper evaluates the potentials and vulnerability of the Sombreiro Warri Deltaic Plain soils using physical properties. A total of 52 genetic horizon soil samples were studied in twelve soil profiles located in Akabuka, Obite, Obagi, Omoku, Okwuzi, Aggah and Umuoru-Ndoni areas.  The soils have predominantly Loamy sand and sandy loam textures on the surface (about 80% of all the studied locations).  Sand content had a range of 220 – 850g/kg with a mean of 515g/kg.  Clay content in the area varied from 140 – 580g/kg, with a very gradual increase with depth in few pedons. The highest clay content was observed in the Umuoru / Ndoni 2 profile where clay had a range of 470 – 580g/kg followed by Umuoru/Ndoni 1 profile with a range of 210 – 270g/kg and a mean of 245g/kg.  The range in particle density for the soils was 2.10 – 2.66gcm-3.  The highest profile mean particle densities were 2.53, 2.50 and 2.43gcm-3 for Umuoru/Ndoni 2, Aggah 2 and Umuoru 1 respectively while the lowest mean values were Obite 1 (2.33), Akabuka 2 (2.33) and Obagi 1 (2.30gcm-3). About 50% of the soils had their particle density between 2.35 and 2.46gcm-3.   The lowest mean values for different pedons were obtained in Umuoro/Ndoni, Obiafu and Aggah pedons with 1.38, 1.42, 1.43 and 1.44gcm-3 respectively while the highest relatively higher values of 1.61, 1.62 and 1.64gcm-3 were obtained in Obite 1, Obagi 1 and Obagi pedons respectively.   Surface horizons generally had lower bulk density values in most of the pedons.  Aggregation in macro aggregate fraction was high in Obagi II, Omoku 1 and Okwuzi.  Aggregate stability was low with Mean Weight Diameter (MWD) of water stable aggregates of 1.64, 1.36, and 1.23mm for Obagi II, Omoku 1 and Okwuzi respectively. Topsoil and subsoil permeability were very slow ranging from 4.92cmhr-1 to 14.18cmhr-1. Mean soil permeability in the profiles were 4.81, 1.28, 8.66, 1.29 and 0.65cmhr-1 for Obite 1, Obrikom, Obagi 2 and Obuburu, respectively.

Keywords: Soil permeability, macro-porosity, Water stable aggregates, Water holding   capacity, Soil Vulnerability

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