id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
esrj-21200	Batayneh, Awni T.	MAPPING SUBSURFACE FORMATIONS ON THE EASTERN RED SEA COAST IN JORDAN USING GEOELECTRICAL TECHNIQUES: GEOLOGICAL AND HYDROGEOLOGICAL IMPLICATIONS	2007	11	.pdf	application/pdf	5130	231	55	Among the four types of curves, Type I and Type II curves show similar shape of field curves with layer resistivities decreasing with depth such that ρ1>ρ2>ρ3. Based on the lithological log from the K3028 borehole, the geological interpretation of the geoelectrical model for VES 4 and VES 5 (Fig. 2) is: (i) a resistive layer (500-1700 ohm-m) with variable thickness and moisture content at the surface, which consists of a mixture of gravel, silt, and sand; (ii) a thick clay and clayish sand layer having resistivity values of 30 to 40 ohm-m; and (iii) a saturated sandy layer with saline water having resistivity values of 1 to 10 ohm-m. FIELD RESULTS ANALYSIS OF VES CURVES	cache/esrj-21200.pdf	txt/esrj-21200.txt