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Open Access Article

1 - Assessment of interpretation methods to calculate aquifer transmissivity from single-well step drawdown aquifer test
Hatefi Etebari Delkhahi Gholam Abbas Fanaei Kheirabad Shahsavari

Since the measured well drawdowns in a single well test does not reflect the aquifer head loss and covering linear and nonlinear well losses, the calculations based on the observed head loss from a pumping well, cannot get a precise estimate of the hydrodynamic paramete More

Since the measured well drawdowns in a single well test does not reflect the aquifer head loss and covering linear and nonlinear well losses, the calculations based on the observed head loss from a pumping well, cannot get a precise estimate of the hydrodynamic parameters of the aquifer. But when an inexpensive and rapid estimation of aquifer transmissivity is required, using the collected data from a single pumping well is amongst the attractive options. Several methods for estimating borehole loss components has been proposed by various researchers. In this study, methods proposed by Eden-Hazel, Hantush-Biershenk, Kasinow, Miller-Weber and Karami-Younger; suggesting to calculate well loss component (CQn) were assessed to determine the transmissivity of the aquifer using measured head losses from both the pumping well and the adjacent piezometer from some aquifer tests conducted on a number of exploration wells of Khorasan (Razavi and Southern) provinces. The calculated well loss components using Eden-Hazel, Hantush-Biershenk, Kasenow and Miller-Weber methods has a significant difference to the simulated well losses using piezometric data. Karami-Younger method has been able to calculate the CQn value more accurately, about 25% to the simulated value. However, an accurate CQn estimate did not necessarily concluded to an acceptable aquifer transmissivity calculation. In the other words, the results of implementation of this method is more sensitive in sediments with high permeability and lower well losses. Manuscript profile

Open Access Article

2 - Determination of stress state and tectonic regime changes in the brittle structures of Chah Yusuf Mountain (East of Gonabad)
فرهاد زارعی Ghaemi Ghaemi

In this study, structural elements, such as faults and fractures and their formation mechanisms and relationships with tectonic regime of Chah Yusuf Mountain in East of Gonabad city have been recognized and discussed. Their relation with regional fractures, based on dat More

In this study, structural elements, such as faults and fractures and their formation mechanisms and relationships with tectonic regime of Chah Yusuf Mountain in East of Gonabad city have been recognized and discussed. Their relation with regional fractures, based on data’s from satellite image process and field data, is also shown. Major faults in this area were identified by using fault plain features such as striations, stretching vein and cumulative steps of minerals that helped us to determine fault mechanisms. In general, faults were oriented in three main directions: 1) Reversed faulting along N90-120˚, 2) Right lateral strike –slip faults along N140-160˚ and 3) Normal faults along N0-15˚. Based on the obtained data and using the inversion method, the orientation of the principal stress axes (σ1، σ2 and σ3) and the ratio of the principal stress differences R in the studied area were analyzed. The results showed two different tectonic regimes in the formation of regional structures: 1) Compressive tectonic regime, major stress along NNE-SSW, which generated structures of folds and reversed faults. 2) Shear tectonic regime, compressive stress along NE_SW and tensile stress line NW-SE, which generated structures such as strike-slip faults, normal faults, vein and tensile fracture. So, the major stress direction in this region is NNE-SSW, which shows its relation to the Late Cenozoic Arabia –Eurasia oblique continental collision. Manuscript profile

Open Access Article

3 - Hydrogeological assessment of Aghajari Formation springs in Masjed Soleyman and Lali area, north-east of Khuzestan Province
مهدی نخستین مرتضوی Mojtaba Tavakoli KamkarRohani Bijan Maleki

The study area with considerable sandstone outcrop is located north-east of Khuzestan province. The aim of this study was to investigate hydrogeological status to find out factors affecting the springs discharge rate. To reach the goal, the stratigraghy, lithology and s More

The study area with considerable sandstone outcrop is located north-east of Khuzestan province. The aim of this study was to investigate hydrogeological status to find out factors affecting the springs discharge rate. To reach the goal, the stratigraghy, lithology and structural assessments were undertaken in the area, and also water sample collection was carried out. The results indicated that there is a positive correlation between springs occurrence and fracture density. The data also revealed that in areas where sandstone thickness is remarkable and fractures well developed, aquifer reservoir as well as spring discharge is promising. The hydrochemical data showed that water quality is controlled by stratigraphy. Correlation between sulfate and calcium ions (R=%90) proves that gypsum and anhydrite dissolution process, caused sulfate water type in the study area. Manuscript profile

Open Access Article

4 - A comparison of Calculated Fixed Radius and Numerical Model Methods to delineate drinking water wellheads protection area in Yaft Abad district, Tehran
بهزاد دلخواهي

Delineation of wellhead protection area is an important component of groundwater protection strategies to prevent probable environmental and health hazards. In this study, besides describing the calculated fixed radius (CFR) and the numerical model methods to determine More

Delineation of wellhead protection area is an important component of groundwater protection strategies to prevent probable environmental and health hazards. In this study, besides describing the calculated fixed radius (CFR) and the numerical model methods to determine the wellhead protection area, in order to compare of the methods, were used from data of eight number of drinking water wells in Yaft Abad district of Tehran. For this purpose, overlapping rate of CFR and numerical model protection areas in GIS environment were analyzed. The overlapping results show increasing distance from the wells, the effectiveness and accuracy of CFR method decreases rapidly. In the 50 days time of travel overlay, 88 percent of the numerical model areas are captured by the CFR areas. While in the 10 years overlay, only 41 percent of the numerical model areas are captured by the CFR areas. When time, money and data are limited, the Calculated Fixed Radius method is an acceptable method only to delineate the 50 days time of travel protection areas. Manuscript profile

Open Access Article

5 - Determination of parental melt nature and evolutions of volcanic rocks in Sarchah geological map area (southern Khorasan) based on isotopic data
Esmaeil Allahpour Mansor VosoghiAbedini Seyed Mohamad Pourmoafi

The 1/100000 geological map of Sarchah area in southern Khorasan province lies at 59˚,30′ to 60˚east longitude and 33˚to 33˚,30′ north latitude. The plain is covered by a wide spectrum of volcanic rocks with a compositional diversity from basic to acidic. In this More

The 1/100000 geological map of Sarchah area in southern Khorasan province lies at 59˚,30′ to 60˚east longitude and 33˚to 33˚,30′ north latitude. The plain is covered by a wide spectrum of volcanic rocks with a compositional diversity from basic to acidic. In this research he parental melt's nature and evolutions via isotopic studies and measurements were studied t. Isotopic correlation plots of 143Nd/144Nd versus 87Sr/86Sr (Zindler and Hart, 1986) showed that extrusive igneous rocks found in this area were originated from those parts of mantle affected by subducted lithospheric slab or metasomatized by crustal substances. As a result, it is necessary to consider the role of parameters such as crustal mingling in dasitic-rhyolitic rocks formation Rhyolitic rocks are significantly affected by crustal materials. These rocks are characterized by higher levels of 87Sr/86Sr and lower levels of 143Nd/1444Nd. Manuscript profile

Open Access Article

6 - Effects of the inclination of parallel no flow boundaries on the time- drawdown curves around a pumping well in a confined bounded aquifer
Arash Nadri ezatolah ghanavati Nasrolah Kalantari

The image well theory was used in the study of no flow boundaries effects on the drawdown around pumping wells. Most studies are concentrated on the vertical no flow boundaries, while, in some cases these boundaries are not vertical and have inclinations. To the best of More

The image well theory was used in the study of no flow boundaries effects on the drawdown around pumping wells. Most studies are concentrated on the vertical no flow boundaries, while, in some cases these boundaries are not vertical and have inclinations. To the best of the authors knowledge, the problem of the inclined no flow boundaries has not been studied yet. The effects of the parallel no flow boundaries inclination on the drawdown around pumping wells in bounded aquifers is studied here. The time-drawdown data for vertical boundaries have used the numerical simulation and also the image well theory. The effects of inclination of the boundaries were only considered using the numerical simulation. The results of numerical simulations and image well theory for vertical no flow boundaries were matched completely. The computed drawdown for observation well in the models with inclined and vertical no flow boundaries used to compute the difference between them. The difference between these cases depends on the distance between the boundaries (width of the aquifer) and the inclination value. The results showed that in large widths and low inclinations, the computed drawdown in aquifers with vertical boundaries are almost similar with the computed drawdown in aquifers with inclined boundaries and the differences can be neglected. In the other words, the difference between the vertical and inclined cases in smaller widths is so high that even in the low inclinations, the differences can't be neglected. It can be concluded that the image well theory as we know, cannot be used in inclined no flow boundaries. Manuscript profile

Open Access Article

7 - Ability of Felmann wells to improve the physical and microbial parameters of river water
Mojtaba G.Mahmoodlu Mostfa Seyed Seyd Mostafa Khezri Gholam Abbas Fanaei Kheirabad

Riverbank filtration can be used as an effective and low-cost method for water treatment of rivers for drinking purposes. In alluvial land consisting of loose sediments (e.g., sand or gravel) with a water table near land surface, one of the most economical methods for e More

Riverbank filtration can be used as an effective and low-cost method for water treatment of rivers for drinking purposes. In alluvial land consisting of loose sediments (e.g., sand or gravel) with a water table near land surface, one of the most economical methods for extracting water in large volumes is the use of wells with large diameter such as Felmann Well. In this study, we investigated the effect of Felmann Wells and riverbank filtration process on improving the water quality parameters of surface water. For this, Doogh River and a Felmann Well were sampled simultaneously within a 5-month period. SPSS software and T-tset were used to determine the significant difference between data obtained from chemical analysis. Comparison of water quality parameters of Doogh River and Felmann Well showed that riverbank filtration can play an important role in reducing the physical and biological parameters of water in Felmann Well drilled near the river. For drinking water purpose, the water quality of both Doogh River and Felmann Well was investigated using WQI (Water Quality Index). Hence, the WQI for Doogh River water varied from 50 to 57, which indicated the average quality of the water of the Doogh River. While, WQI value varied from 64 and 75 for the Felmann well representing a good water quality in the well. Results of this study showed that the Felmann wells which were drilled near the riverbank can play an important role in improving the water quality parameters of surface water for drinking purposes. Manuscript profile

Open Access Article

8 - Analysis of stress regime in Shah Deniz oilfields and wellbore stability, in south Caspian Sea basin
Parvaneh Alizadeh Saeid Mohammad Hassanpour sedghi Ali Kadkhodaie Malek Mohammad Gity

Wellbore instability is one of the main problems during drilling of oil and gas wells. Analyzing and wellbore instability prediction is important. In-situ stress measurement and stress regime are important for stability studies. This study was carried out in one of the More

Wellbore instability is one of the main problems during drilling of oil and gas wells. Analyzing and wellbore instability prediction is important. In-situ stress measurement and stress regime are important for stability studies. This study was carried out in one of the oilfields in the south Caspian basin in Iran. The compressional stress regime in the studied field was determined based on regional stress indicators and larg scale tectonic observations. . This study presented the effect of borehole inclination and azimuth on borehole stability under reverse fault regimes. The magnitude of stresses was determined from measured sonic velocities, density log and predicted pore pressure utilizing the Eaton method. In this study, the modified Lade model have been utilized to perform stability calculation for different inclinations and azimuths. In this study, to perform stability calculation with the use of STABview software is presented. It is shown that drilling wells parallel to maximum in-situ horizontal stress (NE-SW) causes less stability problems. The results of this study could help in the mitigation and/ or prevention of wellbore stability issues in this oilfield. Manuscript profile

Open Access Article

9 - The relationships between diagensis, fracture, distribution of matrix porosity, and well productivities in Bangestan reservoir of Ahwaz field
Mehdi Khoshnoodkia محمد حسين آدابي Mahboubeh Hooseni-barzi Mehdi Khoshnoodkia

Ahwaz Bangestan reservoir (Ilam and Sarvak formations with approximately 1000 meter thickness) were deposited in the Upper Cretaceous period, which is deposited in different sedimentological and tectonic situations. Ahwaz Bangestan reservoir is divided into four reservo More

Ahwaz Bangestan reservoir (Ilam and Sarvak formations with approximately 1000 meter thickness) were deposited in the Upper Cretaceous period, which is deposited in different sedimentological and tectonic situations. Ahwaz Bangestan reservoir is divided into four reservoir zones (C-E-G-I) which are separated by zones of dense limestone (A-B-D-F-H). This reservoir is formed due to repeating shallowing upward of shoal-bar to lagoonal facies with distribution of rudist debris, with the exception of younger sequence which belongs to deeper environment. Back shoal facies show frequent depositional changes in vertical and horizontal directions in zones C3-E-F-G-I, the changes which can be seen in reservoir. Furthermore, the effect of basement faults, with trend nearly N-S in Ahwaz Bangestan reservoir, resulted in changes of ancient paleogeography. These changes had an important effect on diagentic changes, depositional setting, and finally productivity in conventional and carbonate fractured reservoirs. Matrix porosity is fabric selective in zones C3-E-G-and I. So, grainstone, and packstone facies have better reservoir quality than wackestone and mudstone facies. Diagensis and meteoric waters affected the top of every exposure cycles, and caused the best reservoir quality in grainstone, and packstone facies and productivity of wells. But, zone C1 of Ahwaz Bangestan reservoir (chalky limestone) experienced dominantly solution and leaching, which caused an increase in matrix porosity, but little changes in permeability. Furthermore, the open fractures developed in zones E, F and G which are located in the central and southern parts of the field. Existence of open fractures are confirmed by mud losses, analysis of sedimentary structure and dynamic reservoir data. Increase of mud losses in some area of limestone zones (D, F, and H) could be an indication of vertical relationship of two reservoirs and absence of sedimentological barrier in these areas. Manuscript profile

Open Access Article

10 - Comparison of hydrothermal alteration features (zones) of Torud-Chah Shirin magmatic Arc in north and south of the Torud village using Aster image and chemical analyses
Masoud Akhyani Mahdi Kharghani Farhang Sereshgi Morteza rahimi

Torud - Chah Shirin volcanic-plutonic complex, related to Eocene series, is located about 130 kilometers south of Shahrood, in the south and north of Torud village. This zone is located in 54˚20' to 55˚20' east longitude and 35˚10' to 35˚40' north latitude. The presence More

Torud - Chah Shirin volcanic-plutonic complex, related to Eocene series, is located about 130 kilometers south of Shahrood, in the south and north of Torud village. This zone is located in 54˚20' to 55˚20' east longitude and 35˚10' to 35˚40' north latitude. The presence of several mineral occurrences, especially base metal veins of epithermal origin and the intrusion of igneous acidic to intermediate bodies in volcanic rocks of the area caused different alternation and mineralization in some parts of the area and increased the economic importance of the magmatic complex for geological studies. False color composites (FCC), band ratios (BR) and spectral angle mapping (SAM) which were performed on ASTER dataset for discrimination of alteration of argillic, advanced argillic, phyllic and prophyllitic zones and evaluation of results by XRD analysis, are the fundamental information for this research. The field studies and XRD analyses of different zones resulted in adaptation with logical operator algorithms and revealed unremarkable volcanic alteration zone in the south of Torud, in comparison with volcanic zone in the north of Torud. In addition, altering in threshold of algorithm band ratio can be used to find better results in discrimination of argillic and phyllic alterations. Then based on the presence of indicator minerals of advanced argillic alteration in the north of Torud, like alonite and prophillite, the optimal threshold for discrimination of this zone from argillic zone by logical band ratio algorithm was determined. The results were evaluated as acceptable, compared to field study. On the other hand, spectral character of remarkable minerals of this zone, like chlorite and epidotite, in band ratio of Aster 8(9+7) with threshold of 2.3, is reported appropriate for land surveying of proplitic zone in the north and south of Torud village. Manuscript profile

Open Access Article

11 - mythical places in folktales
Sara Chalak

Mythical thought is a kind of worldview that has always saved his situation in humans mind. Mythical idea introduce itself by divide the phenomena of the world into sacred and unholy. Locality is an important mythical subject that differ from modern man’s thinking about More

Mythical thought is a kind of worldview that has always saved his situation in humans mind. Mythical idea introduce itself by divide the phenomena of the world into sacred and unholy. Locality is an important mythical subject that differ from modern man’s thinking about place. Mythical place differ from its surrounding because it is sacred. It may be an archetype like mount or fountain, or may be it has become sacred because of the unworldly object. It has influential power to characters.it can change characters. Folktale as an old type of oral literature contain the insight, philosophic thought and life style of past human being. One of the mythical subject in folktales is locality. This places cause of the relationship with the transcendental affairs, consider as a mythical place. Most of characters in folktale, change mentally by being there and their destiny change. In this article, we tried to use the theories of great mythologists such as Mircea Eliade and Ernest Cassirer to analyze e few sets of folktales. For this purpose, the places such as mount, fountain, sea, river, garden, well were investigated.and their mythical modality was examined. my research method in this article is descriptive and analithical. . Manuscript profile

Open Access Article

12 - A Semi-Central Method to Improve Energy Saving in Real Wireless Sensor Networks Using Clustering and Mobile Sinks
Fatemeh Sadeghi Sepideh Adabi Sahar Adabi

Applying a hierarchical routing approach based on clustering technique and mobile sink has a great impact on reducing energy consumption in WSN. Two important issues in designing such an approach are cluster head selection and optimal allocation of mobile sinks to criti More

Applying a hierarchical routing approach based on clustering technique and mobile sink has a great impact on reducing energy consumption in WSN. Two important issues in designing such an approach are cluster head selection and optimal allocation of mobile sinks to critical regions (i.e., regions those have low remaining energy and thus, high risk of energy hole problem). The limited number of mobile sinks should be utilized due to a high cost. Therefore, allocating the limited number of mobile sinks to the high amount of requests received from the critical regions is categorized as a NP-hard problem. Most of the previous studies address this problem by using heuristic methods which are carried out by sensor nodes. However, this type of solutions cannot be implemented in real WSN due to the sensors’ current technology and their limited processing capability. In other words, these are just theoretical solutions. Consequently, a semi-central genetic algorithm based method using mobile sink and clustering technique is proposed in order to find a trade-off between reduction of computation load on the sensors and increasing accuracy. In our method, lightweight computations are separated from heavyweight computations. While, the former computations are carried out by sensors, the latter are carried out by base station. Following activities are done by the authors: 1) cluster head selection by using effective environmental parameters and defining cost function of cluster membership, 2) mathematical modeling of a region’s chance to achieve mobile sink, and 3) designing a fitness function to evaluate the fitness of each allocation of mobile sinks to the critical regions in genetic algorithm. Furthermore, in our activities minimizing the number and length of messages are focused. In summary, the main distinguishing feature of the proposed method is that it can be implemented in real WSN (due to separation of lightweight computations from heavyweight computations) with respect to early mentioned objectives. The simulation results show the better performance of the proposed method compared to comparison bases. Manuscript profile

Open Access Article

13 - A comprehensive study of shale intervals of Burgan Formation: implications for borehole stability
Mohammad سلیمانی سعیده رعیت دوست

Abstract This aims of this study is to characterize the Shale intervals of Burgan Formation from a borehole stability point of view. This paper describes the process and workflow for data-acquisition and interpretation in a shale formation characterization program an More

Abstract This aims of this study is to characterize the Shale intervals of Burgan Formation from a borehole stability point of view. This paper describes the process and workflow for data-acquisition and interpretation in a shale formation characterization program and demonstrates not only the benefits of acquiring specific data, but also highlights the uses of the data to aid the exploration decision process. The next purpose of this paper is to provide a research process that can be applied in similar geological settings. In the study process, we collected a complete set of information and samples from the field and presented a detailed case study, including laboratorial studies of formation samples and interpretation of the information. Available samples and information sources from Burgan Formation include drillhole cores. The minerals were defined by direct and indirect methods. Bulk XRD analyses performed on core samples showed presence of traces of clay minerals. For determination of the exact clay mineral type, clay minerals were extracted and treated by heat and ethylene glycol saturation. Treated samples were subjected to XRD analyses. Interpretation of the natural gamma spectrometry logs allowed the determination of the type and content of clay minerals. In a next step, in order to study the distribution of minerals types, SEM photomicrographs and Cation exchange capacity (CEC) of the samples were carried out. The results revealed that shale intervals of Burgan Formation are not expandable clays. The instability problem cannot be completely solved by drilling fluid design. The study shows, different approached methods reached the same results. Manuscript profile

Open Access Article

14 - Correction of measured vitrinte reflectance data using the "Fluorescence Alteration of Multiple Macerals" (FAMM) and their application to Well Binak #4 one-dimensional thermal maturity modeling
Mohammad KassaieNajafi Faramarz Shabani Maryam Mirshahani Beyok Ghorbani Arsalan Zenalzadeh

Reflectance of maceral constituents of kerogens, particularly vitrinite (Ro%), commonly used in petroleum exploration, is a very important indicator for determining degree of thermal maturity and investigating status of hydrocarbon generation. Although in vitrinite r More

Reflectance of maceral constituents of kerogens, particularly vitrinite (Ro%), commonly used in petroleum exploration, is a very important indicator for determining degree of thermal maturity and investigating status of hydrocarbon generation. Although in vitrinite reflectance profiles maturity generally increases with increasing depth of burial, basin modelers often experience problems when modeling thermal maturity using vitrinite reflectance data measured by using reflected light- photometer microscopes. The problem of reduced vitrinite reflectance mainly arises due to reflectance suppression in vitrintes. By using the laser Raman microprobe, a new multi-parameter technique called "Fluorescence Alteration of Multiple Macerals (FAMM)" was developed by Australian scientists to solve these problems. In this study, data obtained by application of this method were used to correct suppressed vitrinite reflectance values. In order to examine and demonstrate the extent of suppression effect on modeling results, maturity profile constructed by one-dimensional modeling of Well Binak-4 was calibrated using conventional measured vitrinite reflectance (Ro%) and FAMM equivalent vitrinite reflectance (EqVR) data and results were compared with present time measured well temperatures. The crucial differences in maturation, transformation ratio, hydrocarbon generation and expulsion resulted from application of these two type data as calibration parameters are discussed and demonstrated using relevant diagrams. Manuscript profile

Open Access Article

15 - The application of clustering methods (MRGC, AHC, DC, SOM) determining permeability carbonate reservoir rocks Ilam Formation in South West Iran
Seyed Ali Moallemi farhad khoshbakht sakineh naghdi

The permeability of reservoir parameters is important in the calculation and modeling reservoir plays a role. Measured directly via cores taken from the reservoir layer can be achieved. But due to the limited amount of core taken in a field and laboratory methods as wel More

The permeability of reservoir parameters is important in the calculation and modeling reservoir plays a role. Measured directly via cores taken from the reservoir layer can be achieved. But due to the limited amount of core taken in a field and laboratory methods as well as high cost; use indirect methods to determine the wells without core permeability is great value. In this study, using clustering methods using petrophysical logs permeability values were measured and analyzed. For this purpose, petrophysical logs Ilam Formation selection of 8 wells and addition of data measured in vitro permeability 3-ring is used to compare the results. Log permeability effective porosity in the well using the parameters A with the core permeability data, estimates and then check the accuracy of estimates, calculations also took place in other fields of study. In the next step, using clustering method, was estimated permeability. Then the results with experimental data and correlation coefficient, the best method is introduced. Manuscript profile

Open Access Article

16 - Extraction effect of deep and semi-deep wells on water table decline and groundwater qaulity parameters in Gorgan Plain
M. Pakdel M. G.Mahmoodlu N. Jandaghi A. Fathabadi Y. Nick Ghojogh

The present study was conducted to investigate the effect of increasing uncontrolled drilling of water wells and subsequent extraction of renewable capacity of Gorgan plain aquifer on the decrease in groundwater level and some water quality parameters in a specific peri More

The present study was conducted to investigate the effect of increasing uncontrolled drilling of water wells and subsequent extraction of renewable capacity of Gorgan plain aquifer on the decrease in groundwater level and some water quality parameters in a specific period of 30 years. For this purpose, the trend of rainfall changes, drilling wells, groundwater level fluctuations, as well as some physicochemical parameters were investigated in the studied period. Data analysis of variance was used to investigate the statistical differences between quantitative and qualitative parameters. The annual changes in drilling of authorized and illegal wells in the province shows an increasing trend in the number of wells drilled in the Gorgan plain, followed by an increase in the volume of water extracted since the early 1980s. The results of statistical studies, histograms of annual changes in groundwater level of deep and semi-deep wells as well as hydrographs of deep and semi-deep aquifers studied show a reduction in groundwater level in both semi-deep and deep aquifers in the study period. Since the average annual rainfall in the study period is almost constant, the drilling of shallow and deep wells followed by uncontrolled abstraction of deep and semi-deep aquifers is the most likely major factor in the decline of groundwater levels in the study plain. Based on the statistical results, a significant difference was observed between most of the physicochemical parameters of semi-deep and deep wells in the old and new periods. However, these changes are greater in semi-deep wells than the deep ones. Also, the two parameters Cl and Na, which are the main factors of water salinity, show the greatest changes. Hydrogeochemical diagrams of plain aquifers show an increase in soluble solids as well as changes in the type and hydrochemical facies of groundwater in the new period. However, the trend of changes in the shallow aquifer is more intense. Manuscript profile

Open Access Article

17 - Improving energy consumption in the Internet of Things using the Krill Herd optimization algorithm and mobile sink
Shayesteh Tabatabaei

Internet of Things (IoT) technology involves a large number of sensor nodes that generate large amounts of data. Optimal energy consumption of sensor nodes is a major challenge in this type of network. Clustering sensor nodes into separate categories and exchanging info More

Internet of Things (IoT) technology involves a large number of sensor nodes that generate large amounts of data. Optimal energy consumption of sensor nodes is a major challenge in this type of network. Clustering sensor nodes into separate categories and exchanging information through headers is one way to improve energy consumption. This paper introduces a new clustering-based routing protocol called KHCMSBA. The proposed protocol biologically uses fast and efficient search features inspired by the Krill Herd optimization algorithm based on krill feeding behavior to cluster the sensor nodes. The proposed protocol also uses a mobile well to prevent the hot spot problem. The clustering process at the base station is performed by a centralized control algorithm that is aware of the energy levels and position of the sensor nodes. Unlike protocols in other research, KHCMSBA considers a realistic energy model in the grid that is tested in the Opnet simulator and the results are compared with AFSRP (Artifical Fish Swarm Routing ProtocolThe simulation results show better performance of the proposed method in terms of energy consumption by 12.71%, throughput rate by 14.22%, end-to-end delay by 76.07%, signal-to-noise ratio by 82.82%. 46% compared to the AFSRP protocol Manuscript profile

Open Access Article

18 - Depositional Environmental Analysis of Shally Units of Pabdeh-Gurpi Formation and Clay Minerals Effect on Wellbore Stability, Aghajari Oil Field
بهمن سلیمانی Zahra Dehghani

<!-- [if gte mso 9]><xml> <w:WordDocument> <w:View>Normal</w:View> <w:Zoom>0</w:Zoom> <w:TrackMoves/> <w:TrackForm More

<span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">This research is related to detect of clay minerals and geochemical changes of Pabdeh-Gurpi shale formations and their role in borehole instability in Aghajari oil field. For this purpose, these formations were investigated using NGS well log (one well ring), X-ray diffraction method (XRD) and XRF analytical method (11 samples from two wells). In the NGS log, the detected minerals are illite, montmorillonite, mixed layer, glauconite and feldspar. In the XRD method, clay minerals illite, montmorillonite, mixed layer, chlorite and kaolinite were identified in order of abundance.These minerals due to their sensitivity to react with water causes the instability of the borehole. The high ratio of Si/Al and changes of Ti and high level of Fe3+ and Mg are also a sign of the widespread presence of illite, chlorite and montmorillonite in the mentioned formations.   <span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">The changes of major and trace elements compared to Al2O3 except for MnO, CaO, and P2O5 showed a positive linear relationship. The changes in the amount of Fe2O3 show the oxidizing conditions in the upper part of the base, but the reducing conditions towards the upper side. Based on the amount of iron, manganese and vanadium, the sediments were formed under conditions of reduction, non-sulphide reduction Eh and medium to low pH. Variations in Th/U ratio (1-4.5) indicate marine to transitional environments. The existence of horizons rich in organic matter (more than 2%) confirms the reduction conditions.   <span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">Based on the low values of the Zr/Rb ratio, the sediments in the upper and lower parts are finer than the middle part of the grain. The relative accumulation of biogenic carbonate along with the shale is periodic and is reflected in the changes in the (Zr+Rb)/Sr ratio. Based on the Sr/Ba ratio, marine conditions prevail in the lower part and continental and metamorphic and sometimes marine conditions prevail in the upper part of the formation. Oxidation-reduction conditions were also investigated. The values of the V/(V + Ni) ratio of the semi-reduction region, the Ni/Co ratio of the reduction region and the V/Cr diagram show the almost reduction region and in some cases the oxidant conditions. Paleoclimatic conditions at the time of sedimentation based on low values of Rb/Sr ratio (less than 0.14) were completely hot and dry.   Manuscript profile

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