Iran's Looming Water Bankruptcy
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The Iranian Intervention in the Arab States Affairs: Pretension and Facts
European Journal of Social Sciences ISSN 1450-2267 Vol. 57 No 2 November, 2018, pp.255-267 http://www.europeanjournalofsocialsciences.com/ The Iranian Intervention in the Arab States Affairs: Pretension and Facts Abdulrahman Al-Fawwaz Associate Professor Department of Humanities, Al-Balqa' Applied University P.O.Box: 15008 Amman 11134 Jordan E-mail: [email protected]; [email protected] Abstract Iran, being one of the dominating super powers in the region has been known for its aggressive role in the entire world. The Arab region is exclusively recognized as its strategic position and the substantial availability of natural resources. In the past and even today, the west world have been protecting the global interest in the region and throughout the history, hostilities have been flaring up that affected the internal stability and peace situation. Among this, the role of Iran is dominated towards its intervention within the Arab States. The purpose of the paper is to analyze the Iranian interventions in the Arab States affairs. It tends to investigate that the specific conflicts created by Iran and the impact of those conflicts towards the peace and stability of the Arab States. The findings of the paper are obtained through secondary analysis and it reveals that the major intervention done by Iran in the Arab States are towards religious affairs, territorial, and security affairs, political and trading affairs. Moreover, the Iranian intervention is now expanded towards the military intervention in the Arab States as well, which is affecting the political stability of the region. As the present political situation is sensitive; therefore, much of the policy implications are considered weaker due to the fulfillment of state interest and security. -
The IRGC in the Age of Ebrahim Raisi: Decision-Making and Factionalism in Iran’S Revolutionary Guard
The IRGC in the Age of Ebrahim Raisi: Decision-Making and Factionalism in Iran’s Revolutionary Guard SAEID GOLKAR AUGUST 2021 KASRA AARABI Contents Executive Summary 4 The Raisi Administration, the IRGC and the Creation of a New Islamic Government 6 The IRGC as the Foundation of Raisi’s Islamic Government The Clergy and the Guard: An Inseparable Bond 16 No Coup in Sight Upholding Clerical Superiority and Preserving Religious Legitimacy The Importance of Understanding the Guard 21 Shortcomings of Existing Approaches to the IRGC A New Model for Understanding the IRGC’s Intra-elite Factionalism 25 The Economic Vertex The Political Vertex The Security-Intelligence Vertex Charting IRGC Commanders’ Positions on the New Model Shades of Islamism: The Ideological Spectrum in the IRGC Conclusion 32 About the Authors 33 Saeid Golkar Kasra Aarabi Endnotes 34 4 The IRGC in the Age of Ebrahim Raisi Executive Summary “The Islamic Revolutionary Guard Corps [IRGC] has excelled in every field it has entered both internationally and domestically, including security, defence, service provision and construction,” declared Ayatollah Ebrahim Raisi, then chief justice of Iran, in a speech to IRGC commanders on 17 March 2021.1 Four months on, Raisi, who assumes Iran’s presidency on 5 August after the country’s June 2021 election, has set his eyes on further empowering the IRGC with key ministerial and bureaucratic positions likely to be awarded to guardsmen under his new government. There is a clear reason for this ambition. Expanding the power of the IRGC serves the interests of both Raisi and his 82-year-old mentor, Ayatollah Ali Khamenei, the supreme leader of the Islamic Republic. -
ICID Newsletter 2007 2.Pmd
Managing water for sustainable agriculture Also at http://www.icid.org 2007/2 Message from the President his has been a busy the next forum. Also, the partnership This starts with the topic of climate Tfour months for me, agreed between ICID and the World Water change, which is expected to feature moving back to my Council (WWC), signed in Antalya, pro- prominently at the next WWF. Also, it has home in UK after six vides the framework for the two organi- been proposed that IWALC members could years residence in sations to work more closely together in provide useful input to the next UN World India managing Mott addressing water for food issues more satis- Water Development Report that will be MacDonald’s growing factorily at the next forum. I am grateful to issued at the next WWF. ICID as the business there. I have President Hon Bart Schultz in agreeing to IWALC Secretariat, and also as a member been away from home coordinate the topic with WWC and the of UN-Water, has to play a pivotal role in for a lot longer, and other involved organisations. In the this. there is much to do. meantime, President Hon Aly Shady will th head up the task force that will coordinate 4 Asian Regional Conference 5th World Water Forum, Istanbul ICID efforts to contribute to the forum. Well attended and well organised, the 2009 th Liaison with other Water 4 Asian Regional Conference brought us together with the International Network On my way back from India, I spent a Organisations month in New Zealand and then stopped on Participatory Irrigation Management off in Turkey in March for the kick-off Clearly, if ICID is to have greater influence (INPIM), which now has its base in meetings for the next World Water Forum over the programme for the next forum, Islamabad. -
Biden, Congress Should Defend Terrorism Sanctions Imposed on Iran
Research memo Biden, Congress Should Defend Terrorism Sanctions Imposed on Iran By Richard Goldberg, Saeed Ghasseminejad, Behnam Ben Taleblu, Matthew Zweig, and Mark Dubowitz January 25, 2021 During a Senate Foreign Relations Committee hearing to consider Antony Blinken’s nomination for secretary of state, Blinken was asked whether he believed it is in America’s national security interest to lift terrorism sanctions currently imposed on Iran, including sanctions targeting Iran’s central bank, national oil company, financial sector, and energy sector. “I do not,” Blinken responded. “And I think there is nothing, as I see it, inconsistent with making sure that we are doing everything possible – including the toughest possible sanctions, to deal with Iranian support for terrorism.”1 Bipartisan support for terrorism sanctions targeting Iran goes back to 1984, when the United States first designated the Islamic Republic as a State Sponsor of Terrorism. Since then, every U.S. president2 – Republican or Democrat – and Congress have taken steps to reaffirm U.S. policy opposing Iran’s sponsorship of terrorism and tying sanctions relief to Iran’s cessation of terror-related activities. President Joe Biden has pledged to rejoin the 2015 Iran nuclear deal, formally known as the Joint Comprehensive Plan of Action (JCPOA), if Iran returns to “strict compliance” with the agreement.3 Terrorism sanctions on Iran, however, should not be lifted, even if the Biden administration opts to return to the deal, unless and until Iran verifiably halts its sponsorship of terrorism. This memorandum provides an overview of Iran’s past and ongoing involvement in terrorism-related activities, a review of longstanding bipartisan congressional support for terrorism sanctions on Iran, and a list of terrorism sanctions currently imposed on Iran that should not be lifted. -
Build an Aquifer
“It All Flows to Me” Lesson 1: Build an Aquifer Objective: To learn about groundwater properties by building your own aquifer and conducting experiments. Background Information Materials: • One, 2 Litter Soda Bottle An aquifer is basically a storage container for groundwater that is made up of • Plastic Cup different sediments. These various sediments can store different amounts of • 1 Cup of each: groundwater within the aquifer. The amount of water that it can hold is depen- soil, gravel, 1” rocks, sand dent on the porosity and the permeability of the sediment. • Pin • Modeling Clay Porosity is the amount of water that a material can hold in the spaces be- • Water tween its pores, while permeability is the material’s ability to pass water • Labels • 1 Bottle of Food Coloring through these pores. Therefore, an aquifer that has high permeability, like • 1 Pair of Scissors sandstone, will be able to hold more water, than materials that have a lower • 1 Ruler porosity and permeability. • One 8 Ounce Cup Directions You will build your own aquifers and investigate which sediments hold more water (rocks or sand). Students in your class will use either sand or rocks to food coloring food coloring build their models. You will use a ruler to measure the height of your water soil table and compare it to the height of water in other sediments. 8oz.food coloring soil ruler 8oz. ruler measuring cup sand measuring cup soil sand pin 8oz. rulerpin gravel scissors Building Directions food coloring measuring cup sandgravel scissors pin 1. Take a pin and use it to make many holes in the bot- scissors 2-liter soilplastic cup gravel tom of a cup. -
Water and Irrigation System in Qajar Period
Science Arena Publications Specialty Journal of Humanities and Cultural Science ISSN: 2520-3274 Available online at www.sciarena.com 2019, Vol, 4 (2): 43-49 Water and Irrigation System in Qajar Period Sayyed Sasan Mousavi Ghasemi1, Abbas Ghadimi Gheydari2* 1Master of the History of Islamic Iran, University of Tabriz, Tabriz, Iran. 2Associate Professor of History Group, Faculty of Law and Social Sciences, University of Tabriz, Tabriz, Iran. *Corresponding Author Abstract: Qajar dynasty, which came to power in Iran in early years of the 19th century (end of the 12th century AH) inherited a country that, over the previous century, its economic power had been severely degraded due to many domestic problems and chaos as well as foreign wars and aggressions. Agha Mohammad Khan Qajar, through about twenty years of persistent efforts, could restore political cohesion and integrity to the country. As economy of Iran is considered an agricultural economy, this means that in this system, land ownership and irrigation system are among the important affairs. It can be said that from the 1800s to the last years of Qajar period, agriculture has used the same traditional system of ownership and rural relations have remained unchanged. The only difference seen in this regard is formation of cities and presence of villagers living in the city. In Qajar period, especially in the nineteenth century, the country had not yet entered into capitalist relations, and its monetary economy had not grown much, and the prevailing economy, which mainly provided internal needs of the country, was traditional agriculture. It is very difficult to draw an approximate picture of Iran’s agriculture in the nineteenth century or to show general evolutions of the country that have led to its development, because on one hand, the government has left nothing but some minor investigations of conditions of villages and, in practice, there is nothing about statistics but tax papers. -
Farming the Ogallala Aquifer: Short and Long-Run Impacts of Groundwater Access
Farming the Ogallala Aquifer: Short and Long-run Impacts of Groundwater Access Richard Hornbeck Harvard University and NBER Pinar Keskin Wesleyan University September 2010 Preliminary and Incomplete Abstract Following World War II, central pivot irrigation technology and decreased pumping costs made groundwater from the Ogallala aquifer available for large-scale irrigated agricultural production on the Great Plains. Comparing counties over the Ogallala with nearby similar counties, empirical estimates quantify the short-run and long-run impacts on irrigation, crop choice, and other agricultural adjustments. From the 1950 to the 1978, irrigation increased and agricultural production adjusted toward water- intensive crops with some delay. Estimated differences in land values capitalize the Ogallala's value at $10 billion in 1950, $29 billion in 1974, and $12 billion in 2002 (CPI-adjusted 2002 dollars). The Ogallala is becoming exhausted in some areas, with potential large returns from changing its current tax treatment. The Ogallala case pro- vides a stark example for other water-scarce settings in which such long-run historical perspective is unavailable. Water scarcity is a critical issue in many areas of the world.1 Water is becoming increas- ingly scarce as the demand for water increases and groundwater sources are exhausted. In some areas, climate change is expected to reduce rainfall and increase dependence on ground- water irrigation. The impacts of water shortages are often exacerbated by the unequal or inefficient allocation of water. The economic value of water for agricultural production is an important component in un- derstanding the optimal management of scarce water resources. Further, as the availability of water changes, little is known about the speed and magnitude of agricultural adjustment. -
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology
Hydrogeologic Characterization and Methods Used in the Investigation of Karst Hydrology By Charles J. Taylor and Earl A. Greene Chapter 3 of Field Techniques for Estimating Water Fluxes Between Surface Water and Ground Water Edited by Donald O. Rosenberry and James W. LaBaugh Techniques and Methods 4–D2 U.S. Department of the Interior U.S. Geological Survey Contents Introduction...................................................................................................................................................75 Hydrogeologic Characteristics of Karst ..........................................................................................77 Conduits and Springs .........................................................................................................................77 Karst Recharge....................................................................................................................................80 Karst Drainage Basins .......................................................................................................................81 Hydrogeologic Characterization ...............................................................................................................82 Area of the Karst Drainage Basin ....................................................................................................82 Allogenic Recharge and Conduit Carrying Capacity ....................................................................83 Matrix and Fracture System Hydraulic Conductivity ....................................................................83 -
Thesis Development of an Optimum Framework For
THESIS DEVELOPMENT OF AN OPTIMUM FRAMEWORK FOR LARGE DAMS IMPACT ON POVERTY ALLEVIATION IN ARID REGIONS THROUGH SUSTAINABLE DEVELOPMENT Submitted By ALI ASGHAR IRAJPOOR (2004-Ph.D-CEWRE-01) For The Degree of DOCTOR OF PHILOSOPHY IN WATER RESORECES ENGINEERING CENTRE OF EXCELLENCE IN WATER RESOURCES ENGINEERING University of Engineering & Technology, Lahore 2010 i DEVELOPMENT OF AN OPTIMUM FRAMEWORK FOR LARGE DAMS IMPACTS ON POVERTY ALLEVIATION IN ARID REGIONS THROUGH SUSTAINABLE DEVELOPMENT By: Ali Asghar Irajpoor (2004-Ph.D-CEWRE-01) A thesis submitted in fulfilment of the requirements for the Degree of DOCTOR OF PHILOSOPHY IN WATER RESOURCES ENGINEERING Thesis Examination Date: February 6, 2010 Prof. Dr. Muhammad Latif Dr. Muhammad Munir Babar Research Advisor/ External Examiner / Professor Internal Examiner Department of Civil Engineering, Mehran University of Engineering and Technology, Jamshoro ______________________ (Prof. Dr. Muhammad Latif) DIRECTOR Thesis submitted on:____________________ CENTRE OF EXCELLENCE IN WATER RESOURCES ENGINEERING University of Engineering and Technology, Lahore 2010 ii This thesis was evaluated by the following Examiners: External Examiners: From Abroad: i) Dr. Sebastian Palt, Senior Project Manager, International Development, Ludmillastrasse 4, 84034 Landshut, Germany Ph.No. +49-871-4303279 E-mail:[email protected] ii) Dr. Riasat Ali, Group Leader, Groundwater Hydrology, Commonwealth Scientific and Industrial Research Organization (CSIRO), Land and Water, Private Bag 5 Wembley WA6913, Australia Ph. No. 08-9333-6329 E-mail: [email protected] From Pakistan: Dr. M. Munir Babar, Professor, Institute of Irrigation & Drainage Engineering, Deptt. Of Civil Engineering, Mehran University of Engineering and Technology, Jamshoro Ph. No. 0222-771226 E-mail: [email protected] Internal Examiner: Prof. -
Understanding Aquifers: Demonstration Using a Physical Model
Understanding Aquifers: Demonstration using a Physical Model Part I: Aquifers Explained Geology is the science of planet Earth, its history, and all the processes that act on it. Hydrogeology is the branch of geology which studies how water and rocks interact underground, mainly in aquifers An aquifer is a rock unit that holds enough water to supply water to wells. Aquifers can be found in many types of rocks, such as sandstone, conglomerate, unconsolidated sand and gravel, and fractured rocks composed of limestone or igneous rocks. Here at Barton Springs in Austin, Texas, we are standing on top of the Edward’s Aquifer, composed mostly of fractured limestone. These fractured rocks dissolve overtime and can create large, cave-like systems called Karst aquifers. So when you hear the word Karst, think cave. Some of these caves are big, some of them are small. Karst aquifers are different from sedimentary aquifers, where water flows mostly through the gravel and sand grains similar to a sponge. Hydrogeologists use two terms when investigating aquifers—porosity and permeability. Porosity is all the empty pore space inside a rock given in a percent volume. Porosity represents the volume of water a rock formation can potentially hold. Permeability is how well a fluid can flow within the pore spaces of the rock within the aquifer. For water, we describe this property as hydraulic conductivity. For example, clay and rocks like pumice may have high porosity, but because the pores do not connect with each other, the permeability of these rocks is usually low. Layers of low-permeability material such as clay and shale typically act as barriers to groundwater flow and may often function as an aquitard within a groundwater flow system. -
The Influence of Karst Aquifer Mineralogy And
water Article The Influence of Karst Aquifer Mineralogy and Geochemistry on Groundwater Characteristics: West Bank, Palestine Hassan Jebreen 1,* , Andre Banning 1 , Stefan Wohnlich 1, Andrea Niedermayr 1, Marwan Ghanem 2 and Frank Wisotzky 1 1 Hydrogeology Department, Institute of Geology, Geophysics and Mineralogy, Ruhr University Bochum, Universitätsstr. 150, 44801 Bochum, Germany; [email protected] (A.B.); [email protected] (S.W.); [email protected] (A.N.); [email protected] (F.W.) 2 Department of Geography, Birzeit University, P.O. Box 14, Ramallah, Palestine; [email protected] * Correspondence: [email protected]; Tel.: +49-234-322-5387 Received: 31 October 2018; Accepted: 7 December 2018; Published: 11 December 2018 Abstract: This work reports, for the first time, the mineralogical and geochemical characteristics of karst aquifers in the Central West Bank (CWB) catchment in Palestine. It provides an integrated study approach by correlating the geochemistry of the lithology and hydrochemical data of groundwater samples. Mineralogical analysis showed that all of the samples were dominantly composed of either calcite CaCO3 (5–100 wt. %) or dolomite CaMg(CO3)2 (4–100 wt. %), with minor amounts of quartz and feldspar, which is supported by the inorganic carbon content (9–13 wt. %) and hydrochemical composition of the spring water samples. The whole-rock geochemical data indicated that the samples have low contents of trace elements and transition metals. In contrast, the concentrations of alkaline earth elements (Mg, Ca, Sr, Ba) and Mn were high in the rock and groundwater samples. Generally, the trace elements of rock samples with concentrations >10 ppm included Sr (17–330 ppm), Mn (17–367 ppm), Ba (2–32 ppm), W (5–37 ppm), Cr (3–23 ppm), Zn (1.7–28 ppm), V (4–23 ppm), and Zr (1–22 ppm), while the concentrations of all the other trace elements was below 10 ppm. -
Groundwater Movement and Soils
Lesson # 2: Groundwater Movement and Soils Through the activities below, students will learn how different types of soils and soil structure influence groundwater movement. Students will begin to understand how groundwater can become polluted. Activity # 1: “Sand, Gravel & Clay Soils & Groundwater Movement ” Teacher Preparation: Obtain 3 clear plastic containers or cut the tops off of clear plastic pop bottles. Fill one container with sand, the other with gravel and the final container with clay. Allow the students to feel each soil type and look at each container of soil. Have students discuss the differences they see between the 3 soils. Student Discussion Questions: 1. What do you notice about the size of the particles of sand, gravel & clay? Which has the largest particles? The smallest? 2. Ask students what is between the soil particles (spaces). Tell them that the “spaces” between the particles refers to the POROSITY of the soil. Which soil has the largest and smallest spaces? 3. Ask students which soil would allow water to move through the quickest and explain why. Tell them that the term used to describe the rate or speed at which water moves through the soil is called PERMEABILITY. Explain the relationship between porosity and permeability (larger or smaller spaces between the particles of soil results in a faster or slower movement of water through the soil). 4. If you were to construct a well into an aquifer, which of the 3 soils would you choose. Why? (Answer: Gravel. More water can be stored between the large pores and it would be easiest for a well to pump water from a gravel aquifer with large pore spacing.) 5.