19.06.2013 Views

OBEN GAS DEVELOPMENT PROJECT

OBEN GAS DEVELOPMENT PROJECT

OBEN GAS DEVELOPMENT PROJECT

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Table of Contents and Executive Summary<br />

phytoplankton composition and abundance at Jamieson River are similar to what obtains in similar<br />

water bodies in the Niger Delta. The poor occurrence of euglenoids and cyanophytes in the Jamieson<br />

River indicates the unpolluted state of this river.<br />

1.6.7.3 Zooplankton Studies<br />

The zooplankton community of the surface water consisted mostly of Ostracoda and Copepoda. The<br />

Ostracoda were represented by Cytheridella tepida and Stenocypris sp. The Copepoda was made up of<br />

mainly Cyclopoids (Microcyclops varicans). Generally, the zooplankton diversity was very low.<br />

1.6.7.4 Microbial Flora<br />

The heterotrophic bacterial count of water samples of the Oben Field area ranged from 1.1 x 10 6 to 12.5<br />

x 10 6 cfu/ml with low percentage of hydrocarbon utilizers (0.01 to 0.90%). The counts were within the<br />

range usually obtained from unperturbed environment (10 2 -10 6 cfu/ml). The predominant bacterial<br />

species in the water bodies of the study area were Bacillus s. Staphylococcus sp. Pseudomonas sp.<br />

and Escherichia sp.<br />

The fungal counts of water samples from the Oben Field area ranged from 3.1 x 10 5 to 9.8 x10 5 cfu/ml.<br />

The predominant fungal isolates in water samples within the Oben Field area were Mucor sp.,<br />

Cladosporum sp Penicillium sp. and Candida sp. The low ratio of microbial counts to hydrocarbon<br />

utilizers of below 1.0% indicates that there was low total hydrocarbon content in the waters of the study<br />

area.<br />

1.6.7.5 Hydrogeology/Hydrology<br />

The altitude of the Oben Field rises slightly in excess of 50ft above mean sea level. Three (3) chronostratigraphic<br />

units - Agbada, Akata and Benin formation have been identified in the sedimentary building<br />

of the Niger Delta Basin. Sediment thickness in sequence in most basins was Quaternary deposits<br />

characterized with geomorphologic units.<br />

The hydrogeological set-up constitutes of fine medium grain sand aquifers, which were more than 15m<br />

thick (Oben closest depth is between 46-60m). A clay layer ranging in thickness from 3.5-9.0m overlies<br />

the aquifers and the static water level at Oben was low. The ground waters are portable and belong to<br />

the Ca-Mg-CO3 facia type with low concentrations of hydrocarbons (

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!