Origin, mode of formation of uniformity studies on soils of some physiographic units of Halaib and Shalateen area, Egypt (Record no. 52644)

MARC details
000 -LEADER
fixed length control field 02516cab a2200313Ia 45 0
001 - CONTROL NUMBER
control field u200046
003 - CONTROL NUMBER IDENTIFIER
control field SIRSI
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 120508s2004 ua ss b eng d
040 ## - CATALOGING SOURCE
Original cataloging agency EAL
041 ## - LANGUAGE CODE
Language code of text/sound track or separate title eng
Language code of summary or abstract ara
090 ## - LOCALLY ASSIGNED LC-TYPE CALL NUMBER (OCLC); LOCAL CALL NUMBER (RLIN)
Classification number (OCLC) (R) ; Classification number, CALL (RLIN) (NR) ART ZJAR V31 No4B 4
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Hassanein, A. E.
240 10 - UNIFORM TITLE
Uniform title Zagazig journal of agricultural research, 2004 v. 31 (4B)
Medium [electronic resource].
245 10 - TITLE STATEMENT
Title Origin, mode of formation of uniformity studies on soils of some physiographic units of Halaib and Shalateen area, Egypt
Medium [electronic resource].
246 15 - VARYING FORM OF TITLE
Title proper/short title دراسة أصل وطبيعة وتكوين ومدى تجانس أراضى بعض الوحدات الفيزيوجرافيه فى منطقة حلايب وشلاتين - مصر.
300 ## - PHYSICAL DESCRIPTION
Extent p.1677-1698.
504 ## - BIBLIOGRAPHY, ETC. NOTE
Bibliography, etc. note Includes references.
520 ## - SUMMARY, ETC.
Summary, etc. This investigation was perfomed using the soils of Halaib and Shalateen area in order to evaluate their genesis and degree of homogeneity. Accordingly, eight soil profiles were selected to represent the main physiographic units of this area. The grain size distribution indicates that these soils are mainly coarse texture (sand to sand clay loam). Moreover, the statistical size parameters indicate that these soils are formed by water sediments which mainly transported by rivers and tractive, and turbidity currents, strongly coarse to coarse skewed, very platy to platy and mesokurtic. Mineralogical composition of the sand fraction reveal that the light fraction is generally dominated by quartz with less pronounced amounts of feldspars. The heavy minerals are composed essentially of opaques followed by pyrcboles, (pyroxene + amphipoles). Epidote, zircon, tourmaline and rutile are detected in moderate amounts, while staurolite, garnite, kyanite, silimailite, biotite, monazite and andolusite occur in variable little amounts. Uniformity and weathering rations indicate that these soils are heterogeneous either due to their multiorigin or due to subsequent variations along the course of sedimentation, thus the soils are considered young from the pedological point of view.
546 ## - LANGUAGE NOTE
Language note Summary in Arabic.
596 ## -
-- 1
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Soil formation
Geographic subdivision Egypt.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Soil geomorphology.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element Soil profiles.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Grais, Y. L.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Behiry, E. M. K.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Khider, M. H.
773 0# - HOST ITEM ENTRY
Title Zagazig Journal of Agricultural Research.
Related parts 2004.v.31(4B)
International Standard Serial Number 1110-0338
Control subfield nnas
Record control number u158356
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier <a href="http://nile.enal.sci.eg/EALE/2004/ZJAR/3104/4b/1677.pdf">http://nile.enal.sci.eg/EALE/2004/ZJAR/3104/4b/1677.pdf</a>
Public note Full Text Article.
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type Articles
Source of classification or shelving scheme Library of Congress Classification

No items available.


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