الخصائص المورفومترية لحوض أبو خمسة غرب النجف وأثرها في النشاطات البشرية
رسالة مقدمة إلى كلية التربية للبنات بجامعة الكوفة
كجزء من متطلبات درجة الماجستير في الجغرافية
من قبل
وفاء حميد حسن الفتلاوي
بإشراف
الأستاذ الدكتور
عايد جاسم حسين الزاملي
The Morphometeric Characteristics
of Abu-Khamsah Basin to the West of and its impacts on human activities
A Thesis
Submitted to the Council of Faculty of
Education for Girls - University of Kufa
In Partial Fulfillment of the Requirements
for the Master Degree of in Geography
By
Wafaa Hameed Hasan Al-Fatlawy
Supervised by :-
Prof Dr .Ayyed Jasim Hussein Al-Zamili
Januaru 2019 A.D - Jumada Al-awwal 1440 A.H
Abstract
The study aimed to reveal the variation of the morphometric
characteristics of Wadi Abu Khamesh basin in the west of Al-Najaf. The
study area was divided into three secondary basins. The study included
analysis of the spatial, morphological and surface characteristics of
the valleys. The study concluded that the correlation between
hydrological and morphometric variables between these characteristics
and human activity. The study area is located within the lower valleys
and stones of the stable and untwisted region between the two latitudes (
31 22 00 -31 58 45) north and longitude (43 17 00 -44 12 00) east, with
an area of (822.18) km2 , to the West of the province of Al-Najaf
between Al-Rihaymawy basin on the north and Al- Malih basin on the
south. The study found that the most ancient rocks and sediment belongs
to the Eocene era. Its structure located within the stable shelf, Al-
Najaf scope and the block of Salman affected by all the tectonic
movements experienced by the region, which resulted in a series of
cracks( 7 cracks) that affected the direction of the study area basins.
The surface of the study area is a slight slope (2.9 m / km) in a
southwestern direction to the northeast. The study area is characterized
as a dry area within the region, The dry climate, which is more
evapotranspiration on the precipitation and the temperature varies
between summer and winter. It has seasonal rainfall and the Northwest
winds predominate. Its hydrological characteristics are characterized by
surface water which depends on the falling rain and groundwater.
According to their physical and chemical properties, as demonstrated by
the characteristics of natural plant and its types, the geomorphological
processes, including the weathering processes and their effect on the
formation of the earth shapes of the natural properties referred to, The
analysis of the properties of the ponds in the study area analyzed
morphometric. It was found that the ponds passed through the youth
phase. Therefore, the concentration and flow equations were applied and
compared with the measurement of the water flow volume of the basin of
the study area .
The classification of the lands of the study area according to the
geological criteria of the soil and soil form and divided the vegetation
cover into lands (agricultural, saline, wet, rock, spaghetti, and
barren). Hydrological soils were classified into three types. Depth and
concentration of flow in the basin, and then addressed the natural
potentialities that can be used represented by the natural resources of
surface and groundwater and agricultural activity, natural plants and
pastoralism and human settlements , investment of natural resources, the
extent of exploitation through the rehabilitation of transport routes
and interest in the tourist aspect.
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