﻿<?xml version="1.0" encoding="UTF-8"?>
<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns="http://purl.org/rss/1.0/" xmlns:content="http://purl.org/rss/1.0/modules/content/" xmlns:sy="http://purl.org/rss/1.0/modules/syndication/" xmlns:sciepub="http://www.sciepub.com" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:taxo="http://purl.org/rss/1.0/modules/taxonomy/" xmlns:prism="http://prismstandard.org/namespaces/basic/1.2/">
  <channel rdf:about="http://www.sciepub.com/portal/Journals">
    <title>Journal of Geosciences and Geomatics</title>
    <link>http://www.sciepub.com/journal/JGG</link>
    <description>Journal of Geosciences and Geomatics is a peer-reviewed, open access journal that provides rapid publication of articles in all areas of geosciences and geomatics. The goal of this journal is to provide a platform for scientists and academicians all over the world to promote, share, and discuss various new issues and developments in different areas of geosciences and geomatics.</description>
    <dc:publisher>Science and Education Publishing</dc:publisher>
		<dc:language>en</dc:language>
		<dc:rights>2013 Science and Education Publishing Co. Ltd All rights reserved.</dc:rights>
		<prism:publicationName>Journal of Geosciences and Geomatics</prism:publicationName>
		13
		3
		January 2025
		<prism:copyright>2013 Science and Education Publishing Co. Ltd All rights reserved.</prism:copyright>
    <items>
      <rdf:Seq>
        <rdf:li resource="http://pubs.sciepub.com/jgg/13/3/1"/>
<rdf:li resource="http://pubs.sciepub.com/jgg/13/3/2"/>
      </rdf:Seq>
    </items>
  </channel>
  <item rdf:about="http://pubs.sciepub.com/jgg/13/3/1">
<title>
Gravity Modelling and Structural Characterization of the Korosi–Chepchuk Geothermal Fields in Baringo, Kenya
</title>
<link>http://pubs.sciepub.com/jgg/13/3/1</link>
<description>
<![CDATA[Exploration and exploitation of geothermal resources is a very high-risk venture with high upfront costs. Hence, a clear understanding of the subsurface structural controls is more important in the development of a geothermal system. In this study, gravity data was processed to remove all the variations which do not result from the effects of underlying masses. Using the Golden Surfer Software, a grid and bouguer anomaly map was generated. To separate regional and residual anomalies and also remove effects of noise, the gridded data in Geosoft Oasis Montaj Software was subjected to band pass filter, high pass filter, upward continuation and both first order vertical and horizontal derivatives. The respective anomaly maps were plotted and analyzed. Finally, a gravity profile was obtained across the anomaly and 2D forward modelling performed. From the analysis, it was observed that there were two peaks, one at the Korosi and other at Chepchuk which are interpreted as the magma intrusions appearing at the depth of approximately 3km. Linear gravity gradients were also detected trending NE-SW direction which are possibly the Nakaporon and Nagoreti faults. Two target wells expected to be more productive in the area could be decided.]]>
</description>
<dc:creator>
Chelangat  Hellen, Namaswa  Solomon, Munyithya  James
</dc:creator>
<dc:date>2025-09-22</dc:date>
<dc:publisher>Science and Education Publishing</dc:publisher>
<prism:publicationDate>2025-09-22</prism:publicationDate>
<prism:number>3</prism:number>
<prism:volume>13</prism:volume>
<prism:startingPage>52</prism:startingPage>
<prism:endingPage>56</prism:endingPage>
<prism:doi>10.12691/jgg-13-3-1</prism:doi>
</item>
<item rdf:about="http://pubs.sciepub.com/jgg/13/3/2">
<title>
Soil and Their Agronomic Suitability for Cocoa (Theobroma cocoa L.) in South Cameroon Plateau
</title>
<link>http://pubs.sciepub.com/jgg/13/3/2</link>
<description>
<![CDATA[Cameroon is the world's fifth largest producer of cocoa (40,000 hectares of land), which is the main cash crop, employing 75% of farmers in central and southern Cameroon. However, low yields (370 kg. ha-1) have been observed over time due to soil conditions, climate variability, and poor agricultural practices. To this end, a detailed characterization of the soils of the southern Cameroonian plateau will make it possible to optimize yields. Thus, the present study aims to characterize the soils of the Nkolandom locality in order to determine their suitability for cocoa cultivation. The study consisted of conducting a soil survey to open pits, whose horizons were characterized, and samples were taken for laboratory analysis of physicochemical parameters. The evaluation of the suitability of the soil for cocoa cultivation was carried out using the FAO method. Three (03) types of soil were identified: loose soils, hydromorphic soils, and soils on crust, which have morphological and analytical characteristics such as thick, sandy-clay to clayey texture, polyhedral structure, acidic to very acidic pH (4.1 to 5.8), low to moderate CEC content (7.28 to 27.76 cmol kg<SUP>-1</SUP>), and low to very high organic matter content (1.4 to 9.1%). These soils have respective suitability classes S3/Nc,f , Nc,w and Nc,s due to climatic limitations, soil fertility, soil water conditions and soil physical characteristics. Ferrasols have a marginal to unsuitable aptitude due to climate (relative humidity in the driest month), where it is advisable to irrigate the soil in the dry season and use agroforestry systems (SAF), and soil fertility (pH and CEC), where it is more appropriate to correct the soil pH and use cover cropping systems (SCV). Gleysols and Ferrasols on armourstone have an uncorrectable inaptitude due to the waterlogging of these soils and the presence of armourstone where cocoa cannot move its roots well.]]>
</description>
<dc:creator>
Amira  Zainab Mbombo, Lionelle  Estelle Mamdem, Bienvenue  Achille Ibrahim, Denis  Tiki, Lucian  Banakeng, Emile  Temgoua, Dieudonné  Bitom
</dc:creator>
<dc:date>2025-09-29</dc:date>
<dc:publisher>Science and Education Publishing</dc:publisher>
<prism:publicationDate>2025-09-29</prism:publicationDate>
<prism:number>3</prism:number>
<prism:volume>13</prism:volume>
<prism:startingPage>57</prism:startingPage>
<prism:endingPage>66</prism:endingPage>
<prism:doi>10.12691/jgg-13-3-2</prism:doi>
</item>
</rdf:RDF>