Textural Analysis, Erodibility Index Analysis and Hydro Network Pattern Delineation of Eocene Strata, South-Eastern Nigeria

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Chidolue, Chukwudi Cyril
Chidolue, Chukwudi Cyril
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Chidolue
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Chukwudi Cyril
Chukwudi Cyril
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Textural Analysis, Erodibility Index Analysis and Hydro Network Pattern Delineation of Eocene Strata, South-Eastern Nigeria

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Abstract

Detailed field based studies were carried out on Eocene Strata of Nanka Sandstone, unit of Niger Delta. Textural analyses were carried out on twenty-one samples of the rock collected from various units across the study area. Gradistat v.8.0 was used to analyze the data obtained for sieve analysis. TRI-PLOT v. 1-4-2 was used to analyze the data obtained for pebble morphometry. The sieve analysis data were also subjected to the Erodibility Index Analysis (EIA) to estimate Erodibility Tendency (ET). By manual delineation, and the use of ArcGIS, the Hydro Network Pattern (HNP) was carried out. A reflection of a predominant shallow marine depositional environment controlled by tidal influence with its corresponding stratigraphy was observed. Very severe Erodibility Tendency (ET) was predicted based on very high values of Soil Loss (R) through the calculated erodibility indices, direct heavy raindrop impact on the sediments and the Hydro Network Pattern (HNP) which favor intense erosion of the study area. The criticality of this intense accelerated erosion is being factored by the friability and very high sand to clay ratio of Nanka Formation.

References

26 Cites in Article
  1. I Arua,V Rao (1986). New stratigraphic data on the Eocene Ameki Formation, southeastern Nigeria.
  2. I Arua (1990). The trace fossil Teredolites longissimus in calcareous concretions from the Eocene Ameki formation, southeastern Nigeria.
  3. G Bouyoucos (1935). The clay ratio as a criterion of susceptibility of soils to erosion.
  4. T Chinatu (2007). Relative Efficiencies of Erosivity Indices in Soil Loss Prediction in Southeatern Nigeria.
  5. Chiaghanam, O.I,Chiadikobi K.C,Ikegwuonu, O.N,Omoboriowo, A.O (2014). Palynology, Source Rock Potential and Thermal Maturity of Eocene Nanka Formation (Ameki Group) In Anambra Basin: An Investigation of Agulu Lake, South-Eastern Nigeria.
  6. J Dobkins,R Folk (1970). Shape Development on the Tahifi-mi.
  7. O Ekwenye,G Nichols,A Mode (2014). Sedimentary petrology and provenance interpretation of the sandstone lithofacies of the Paleogene strata, south-eastern Nigeria.
  8. O Ekwenye,G Nichols,C Okogbue,A Mode (2016). Trace fossil assemblages in the tide-dominated estuarine system: Ameki Group, south-eastern Nigeria.
  9. R Folk,W Ward (1957). Brazos River bar, a study in the significance of grain size parameters.
  10. R Folk (1974). Petrology of Sedimentary Rocks.
  11. N Hudson (1995). Soil Conservation.
  12. G Lutting (1962). The Shape of pebbles in the Continental Fluviatile and Marine Facies.
  13. E Nwabineli,V Otti (2012). Environmental Effects of Gully Erosion in Nigeria: Case Study of Nanka Community, Orumba North, L.G.A of Anambra State.
  14. C Nwajide (1980). Eocene tidal sedimentation in the Anambra basin, Southern Nigeria.
  15. I Obi,A Mode (2013). Paleocurrent analysis as tool for reservoir property estimation: a case study of Eocene outcrops in Southeastern Nigeria.
  16. I Obiadi,A Onwuemesi,O Anike,N Ajaegwu,E Anakwuba,C Nwosu,E Akpunonu,E Onuigbo,O Onuba (2011). Determining Subsurface Fracture Characteristics from the Azimuthal Square Array Resistivity Survey at Igarra, Nigeria.
  17. C Ali,T Ejiofor,F Ifeanyieze,A Okadi,C Eze,G Eze,F Onah,T Nwakile,C Ugwuoke,R Mgbenka,O Onah,C Nwachukwu,F Ezebuiro,B Omeje,L Ekenta,E Ogbonna (2014). Proximate qualities and lycopene contents of three watermelon (Citrullus lanatus) fruit varieties grown with climate-smart integrated fertilizer management in sandy loam soil.
  18. C Osadebe,T Abam,F Obiora,R Sani (2014). Evaluating the Stability of Gully Walls in Agulu-Nankaoko Gully Erosion Complex Area of Anambra State, Nigeria, using Empirical Approach.
  19. F Pettijohn (1957). Sedimentary Rocks.
  20. E Roose (1977). Application of the universal Soil Loss equation of Wischmeier and Smith in West Africa.
  21. B Sahu (1964). Depositional mechanism from the size analysis of elastic sediments.
  22. C Sames (1966). Morphometric data of some recent pebble associations and their application to ancient deposits.
  23. Shell-Bp (1957). Unknown Title.
  24. K Short,A Stauble (1967). Outline of geology of Niger Delta.
  25. Edmund Sneed,Robert Folk (1958). Pebbles in the Lower Colorado River, Texas a Study in Particle Morphogenesis.
  26. G Visher (1969). Grain size distributions and depositional processes.

Funding

No external funding was declared for this work.

Conflict of Interest

The authors declare no conflict of interest.

Ethical Approval

No ethics committee approval was required for this article type.

Data Availability

Not applicable for this article.

How to Cite This Article

Chidolue, Chukwudi Cyril. 2018. \u201cTextural Analysis, Erodibility Index Analysis and Hydro Network Pattern Delineation of Eocene Strata, South-Eastern Nigeria\u201d. Global Journal of Science Frontier Research - H: Environment & Environmental geology GJSFR-H Volume 18 (GJSFR Volume 18 Issue H1): .

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Issue Cover
GJSFR Volume 18 Issue H1
Pg. 27- 31
Journal Specifications

Crossref Journal DOI 10.17406/GJSFR

Print ISSN 0975-5896

e-ISSN 2249-4626

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GJSFR-H Classification: FOR Code: 040699
Version of record

v1.2

Issue date

March 5, 2018

Language
en
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Detailed field based studies were carried out on Eocene Strata of Nanka Sandstone, unit of Niger Delta. Textural analyses were carried out on twenty-one samples of the rock collected from various units across the study area. Gradistat v.8.0 was used to analyze the data obtained for sieve analysis. TRI-PLOT v. 1-4-2 was used to analyze the data obtained for pebble morphometry. The sieve analysis data were also subjected to the Erodibility Index Analysis (EIA) to estimate Erodibility Tendency (ET). By manual delineation, and the use of ArcGIS, the Hydro Network Pattern (HNP) was carried out. A reflection of a predominant shallow marine depositional environment controlled by tidal influence with its corresponding stratigraphy was observed. Very severe Erodibility Tendency (ET) was predicted based on very high values of Soil Loss (R) through the calculated erodibility indices, direct heavy raindrop impact on the sediments and the Hydro Network Pattern (HNP) which favor intense erosion of the study area. The criticality of this intense accelerated erosion is being factored by the friability and very high sand to clay ratio of Nanka Formation.

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Textural Analysis, Erodibility Index Analysis and Hydro Network Pattern Delineation of Eocene Strata, South-Eastern Nigeria

Chidolue
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Chukwudi Cyril
Chukwudi Cyril

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