Rafidain journal of science

Three different mixtures (sand:clay), (80:20), (70:30) and (60:40), were formed in a cylindrical shape of 50×50 mm, using a semi–dry pressing with 300 kg/cm2 as forming pressure and then fired at 1430˚C. The results showed that the produced semi silica bricks have apparent porosity ranging from 21.3-25% with specific gravity between 2.42-2.93 N/mm2 and having spelling resistance between 15 to 25 cycle. The results show that it is possible to use a mixture of 60:40 sand:clay for the manufacture of semi silica bricks

The local lime has been used as a coagulant and a coagulant aid with ferrous sulfate
in turbidity removal for deferent level of initial synthetic turbidity (25,100,500) ntu. The
study revealed that the lime can effectively be used alone as a coagulant with medium
and high initial turbidity levels (100and500) ntu, And it revealed a better result when it
used as a coagulant aid with ferrous sulfate at low initial turbidity limit 25ntu with a dose
of 20mg/l with 7.5mg/l of ferrous sulfate to get a removal of 93% of turbidity.
Regression analysis has been done and a mathematical model determined for the
variables included in the study, and it found that the most important variable affect to
turbidity removal is the initial turbidity followed by settling time then ferrous sulfate dose
th e n li m e d o se

In this study The Water Quality Index (WQI) has been used to evaluate the ground
water for a group of dug wells in northwest of Mosul city by using Multiplicative
weighted mean method which known Geometric mean method; the study revealed thebadness of ground water in the area for both drinking and irrigation uses; where it fall in
the group five for drinking water and group four and five for irrigation uses, In relating
of stockyard uses the well water is more suitable for this use and it fall in the groups one,
two, three and four for this use. From comparing the WQI of the wells in the area with
the WQI of Tigris River it found that is no big interaction between the river and the
wells.

The twenty one variables (representing climatical, hudrological and
geomorphological factors) of six sub basins forming Wadi Al- Therthar north – west Iraq
was studied to found relation between these variables and amount of runoff.
The area is located geographically between (36°30΄ - 35° 35΄) latitude and (43° 00΄
- 41° 55΄) longitude.amount of runoff from these basins as dependent variable and the other variables as
independent.
Results led to the formulations of mathematical equations which can be use for the
predication of the rate of flow other selected variables.

The Jeribe Formation of Sheikh- Ibrahim area is divided into two parts of variable bedding characters. The lower bedded part comprises carbonated beds of chalky, massive and biogenic limestone. The massive upper part is constituted of hard limestone and dolomitic limestone associated with fringing dolomite breccia. The massive limestone is dominated by blue- green algal buildup, which has been highly dolomitized. Petrographic examination of dolomite in the upper part revealed the following textures: aphanotopic, limpid and mosaic dolomite textures. The inference gained from petrographic evidence point to dolomitization by the mixing zone model.

To display the significance of the remotely sensed data in geological exploration,
ratio images were used to allocate the prospected area of gypsum rocks. Ratioing
operation removes the albedo information and enhances the reflectivity of the cover type
.A combination of ratio images based on the spectral characteristics of gypsum rocks was
selected. This combination consists of (Band4/Ban3), (Band7/Ban1) and (Band7/Ban4).
Gypsum rocks are expected to appears in white tone in ratio images (Band4/Ban3), while
it expected to appears in dark tone in the ratio images (Band7/Ban1) and (Band7/Ban4) .
However, to exploit the capability of ratio images for better discrimination, these ratio
images were combined into a false colors composites which reflect the gypsum rocks in
blue color in ratio images ((Band 4 / Band 3)G, (Band 7 / Band 1)B and (Band 7 /
Band 4)R)). To avoid the false ratio value which appears as result of scattering effective
images portrayed in short wavelength, the raw images were subjected to methods of
image correction. Finally, all the operations of correction and ratioing were programmed
in C++ language. The software is adaptive so that it can be used for any cover type
discriminating using any sensor type.

The Stratigraphy and facies analyses of the unknown calcareous conglomerate unit,
which has recently been brought up by bore holes in Sfaya oil field at north western Iraq,
have been shown that this unit is of “Turonian-Santonian” age. Lithologically,
conglomerate and embedded mudstone lenses at the western and centeral parts of the
field represent the unit. On the other hand, it is represented by conglomerate, which is
interfingering with lagoonal carbonates at the southeastern parts and by thick typicallagoonal carbonate facies, which overlay a tongue of conglomerate extending towards
Ain-Zala oil field. Stratigraphic and facies analyses have indicated that this unit was
deposited in a limited lagoonal environment.

The variation of quality characteristic of Mosul lake, was studied by monitoring the
changes in the physical and chemical characteristics of water through two periods. The
two periods have been chosen during July and November respectively. The changes of
several samples, taken at different depths, were monitored. The changes included,
temperature (T), pH, electrical conductivity (EC), dissolved oxygen (DO), total hardness
(TH), calcium (Ca), magnesium (Mg), sodium (Na), potassium (K), bicarbonate
(HCO 1
3
− ), phosphate (PO 3
4
− ), nitrate (NO 1
3
− ), chloride (Cl) and sulphate (SO 2
4
− ), Crosssections
that represent the changes in the characteristics were shown graphically.
The results have shown that for the July period the changes in temperature has
greater effects on some of the specific characteristics such as pH, DO, (HCO 1
3
− ), and
PO 3
4
− than the others. The effects have produced three strata-zones of different specific
characteristics that synchronize with three strata-zones of different temperatures.
For the November periods the study has shown that the lake is at the beginning of
autumn turnover state. Besides, the study has shown that concentration of (DO) does not
show the overturning process clearly. Also the decrease in the amount of oxygen in the
lake, which in turn, lead to the formation for a reducing environment that increases the
biological pollution inside the lake. In addition, the concentration of dissolved ions will
increase as result of the absence of the self-treatment inside the lake.

The state of Hadramout Governorate South of Yemen is facing serious water crises as a result of its limited natural water resources, and the over-abstraction from the Shihr, Tawilah and Quaternary deposit aquifer systems. The aquifer heads have fallen, giving rise to the problem of seawater intrusion and resulting in the loss of the fresh ground water resources.
A hydrological map showing the spatial distribution and characteristics of three different types of ground water aquifer systems associated with the nature of rock types and permeability in the study area. The physical and chemical analysis from the water resources (AL-Naqaá-Adhibah-Thilah and Fowah) which supply Mukalla and Gail Ba Wazeer zones were tested during the period 17/11/2001 to 27/3/2002. Laboratory analysis showed clear high concentration almost in all the water constitutions. These results are above the values set by the World Organization of Health (WHO) and exceed the Yemeni guidelines for drinking water. The high results are in total dissolved solids (total alkalinity, total hardness, sulphates, manganese and fluorine).
Techniques of water harvesting which was appropriate for this application using remote sensing satellite, taken in 2001, has been analyzed in both descriptive and quantitative geomorphic methods to improve water quality in the area of study a whole, which suffers from high concentration of water constitutions, ending with the adoption of the concept of water harvesting using flash flood in the main drainage basins. So, there is great necessity to give these water resources the superior priority in the future decision planning, to improve ground water aquifer systems in the study area.

In the present geoelectric investigations, the Mosul depression, which lies between the structures of Fadhliya, Bashiqa and Ain Safra in the northeast and Allan and Atshan in the southwest, has been carefully investigated. The Investigation envolved eighty eight depth electric sounding measurements using collinear symmetrical Schlumberger electrode arrangement with maximum C1C2 distance of 1500m.These measurements were distributed over an approximately regular grid covering an area of about 1000 sq.km. Continuous correlation of the layer models with the lithological logs of numerous wells in the area are made.
Detailed analyses of the geoelectrical data and their accurate interpretations showed the existence of a number of folded structures that were unknown previously. Various other, previously suggested structures were affirmed. A number of strike-slip faults were delineated, with oblique slip movement, which is not known previously. A number of block faults (Zagroside and Tauroside blocks) have also been recognized. Therefore, the Mosul depression is a graben created by system of block reverse faulting.

The hydrogeomorphology of Wadi Al-Meleh basin studied quantitatively using
remote sensing data .The studied area is located at northern part of Iraq.
The stages of the study included a preparation of geomorphological maps, followed
by morphometric analysis of twenty-two variables.
These variables represent climatical, hydrogeological and geomorphological factors
for five major sub basins that form Wadi Al-Meleh.The statistical analysis of correlation and regression of these variables applied
where amount of runoff from these basins as dependent variable and the other variables
as independent.
Results shown models, which can be used for the prediction of the rate of flow of
this basin from other selected variables.

Petrographic study of the sandstones of Injana Formation in the well (KH8/9) revealed them to consist dominantly of carbonate rock fragments with subordinate monopoly crystalline quartz, K-Na feldspars fragments, igneous–metamorphic rock fragments and mica, in addition to matrix and cement of variable composition (carbonate, iron oxide, silica and sulphates). These suits of components can be related to provenance overwhelmed by sedimentary rocks with lesser contribution of igneous and metamorphic rocks.
This sandstone is mineralogically and texturally immature and of calclithite variety originated from source rock under colder conditions compared to their semi-arid environment of deposition. The tectonic setting of back – arc attributes as a consequence of plate-collision and overthrusting played a dominate role in sourcing the sediments.

Predicting Three dimention solid model for aquifers in any region is one of the most
important aims for hydrologists to reach. The Electrical investigation data have been usedfor Hamdania region. This data represent the aquifers thickness in electrical sounding
points. AThree dimention computerized solid model was build using the groundwater
modeling system (GMS). This has been done by connecting the aquifer upper points to
make triangular irregular network (TIN), which is repeated for all aquifers in the study
region to make four TINs. By filling between these TINs a 3D solid model was build for
geological aquifers in the study region. The size and the dimentions for all aquifers were
calculated from this model. The volume for Bi Hasan Formation is (21 x 109) m3 while
the volume for Injanah Formation is (136 x 109) m3.

Carbonates of Sinjar Formation (Paleocene-Early Eocene) have been studied along
two exposed sections situated at both limbs of Sinjar anticline. Facies analysis shows the
presence of twenty microfacies, including four facies of boundstone type. The delineated
microfacies indicate that the succession of Sinjar Formation represents a complete reef
system zone. The succession of Sinjar Formation consists of two sedimentary subcyclesThe lower one represented by sandy lime facies of reef slope facies. This reef system is
characterized by a very narrow lagoon and reef zones and limited reef slope zones. This
refers to remnant facies of previous regressive phase, which occurred at the end of
Danian period. The second subcycle represented by the rest of the succession of the
formation. This subcycle is believed to be deposited through regional transgressive phase
during Paleocene to Early Eocene period. This led to the development of reef system with
all reefal environmental zones.