Noticias de ataques y destrucciones en Orihuela durante el período andalusí (ss. VIII-XIII)

Tras resumirse "Los elementos esenciales de la trama urbana de Orihuela", se estudian los principales hechos históricos durante el período islámico de la ciudad de Orihuela "s. VIII-XIII) en que hay noticia de ataques militares a la ciudad y destrucciones : El ataque de los normandos a Orihuela en 245 H ./859 e.C.; Aceifa del califa ‘Abd al-Raḥmān III al-Nāṣir contra Orihuela y sus rebeldes; La "fitnat al-barbar" o guerra civil que acabó con el califato andalusí; El terremoto posterior a 440 H/1048-9 e.C. que asoló toda la vega del río Segura y finalmente la conquista cristiana de Orihuela. Como conclusiones para el estudio del urbanismo musulmán de Orihuela se demuestra que solo hubo destrucciones en el trazado urbano de importancia como resultado del mencionado terremoto que asoló y destruyó las ciudades de Murcia, Orihuela y toda la Vega Baja del río Segura.

Democracy Concepts of the Fundamentalist Parties of Algeria and Tunisia – Claim and Reality

This article discusses democratic elements in early Islamic sources and in the programs of the Algerian FIS (Front Islamique du Salut) and ANNAHDA in Tunesia. According to historic writings, Islam includes the principles of democratic consensus, consultation, and freedom of opinion, and an understanding that the sources of Islamic jurisdiction are subject to interpretation, that the sharia can be changed, and that religious authorities’ power to issue instructions on worldly matters is limited. These are the type of expectations that fundamentalist parties arouse when they speak of an Islamic caliphate as a state system. Against this background, an examination of the political system proposed until 1992 by the Algerian FIS shows that this system would have resulted in a very restrictive form of Islam. An investigation of the political system of the Tunisian fundamentalist leader Rached al-Ghannouchi reveals that the system he proposes may be designated as an Islamic democracy, since it takes into account separation of powers and pluralism of political parties. The head of state would be subject to the law in the same manner as the people. However, it is no liberal democracy, as he categorically rejects secularism, intends to punish apostates, and is only willing to allow political parties that are based on the religion of Islam. His state would only be a state of those citizens who follow Islam, completely neglecting secularist groups. Social conflicts and unrest are thus predetermined.

The Middle East in the shadow of the Islamic State. OSW Point of View Number 52, August 2015

Since June 2014, Islamic State (IS) has been regarded as the principal security threat in the Middle East and one of the most important problems for European and global security. Islamic State, which for many years was just one of many terror organisations with links to al-Qaeda, has succeeded in achieving much more than other similar organisations: it has taken over control of large swathes of territory in Syria and Iraq by military means, created its own para-state structures in that area, and become the greatest civilisational challenge for the region in a century as it established a self-proclaimed caliphate and credibly pledged to expand further on a global scale. Those successes have been accompanied by widely publicised acts of systemic brutality which meets the definition of crimes against humanity. One outcome of these developments is the emergence of an exotic informal alliance to combatthe Islamic State, which has brought together all the states from the Middle East and many from beyond the region. However, contrary to what could have been predicted, after almost a year of the declared war against IS, the Caliphate still holds most of the ground it gained in 2014.

Without an empire: Muslim mobilization after the caliphate

The Caliphate was a fundamental part of Islamic society for nearly 1300 years. This paper seeks to uncover what effect the removal of this institution had on the mobilization of Muslims in several parts of the world; Turkey, Egypt, and British India. These countries had unique experiences with colonialism, secularism, nationalism, that in many ways conditioned the response of individuals to this momentous occasion. Each country’s reaction had a profound impact on the future trajectory of civil society, and the role of Islam in the lives of its citizens. The conclusions of this paper challenge the monolithic depiction of Islam in the world, and reveal the origins of conflict that these three centers of Muslim power face today. Much of the religious narrative now commonplace in Muslim organizations derive from this pivotal event in world history.

The Approach to Daesh in Tunisia: From Bardo to Ben Gardane, aYear of Terror

Starting from a descriptive analysis of the main attacks by Daesh in Tunisia, this article examines the nature and evolution of the terrorist organization in this North African country. Thus, it examines the characteristics and vicissitudes of the attack on the Bardo Museum in March 2015, the attack on the Susa beach in June 2015, the bombing of the Presidential Guard in November 2015 and, finally, the military offensive against the town of Ben Gardane in March 2016. In addition, it presents some previous facts that are relevant in this research, such as the important presence of Tunisian foreign fighters in Syria or Libya, and, in particular, the threat of Daesh in Libya to the Tunisian State

In Situ Observation of the Thermal Decomposition of Weddelite by Heating Stage Environmental Scanning Electron Microscopy

The morphological and chemical changes occurring during the thermal decomposition of weddelite, CaC2O4·2H2O, have been followed in real time in a heating stage attached to an Environmental Scanning Electron Microscope operating at a pressure of 2 Torr, with a heating rate of 10 °C/min and an equilibration time of approximately 10 min. The dehydration step around 120 °C and the loss of CO around 425 °C do not involve changes in morphology, but changes in the composition were observed. The final reaction of CaCO3 to CaO while evolving CO2 around 600 °C involved the formation of chains of very small oxide particles pseudomorphic to the original oxalate crystals. The change in chemical composition could only be observed after cooling the sample to 350 °C because of the effects of thermal radiation.

Thermal decomposition of the synthetic hydrotalcite iowaite

The thermal stability and thermal decomposition pathways for synthetic iowaite have been determined using thermogravimetry in conjunction with evolved gas mass spectrometry. Chemical analysis showed the formula of the synthesised iowaite to be Mg6.27Fe1.73(Cl)1.07(OH)16(CO3)0.336.1H2O and X-ray diffraction confirms the layered structure. Dehydration of the iowaite occurred at 35 and 79°C. Dehydroxylation occurred at 254 and 291°C. Both steps were associated with the loss of CO2. Hydrogen chloride gas was evolved in two steps at 368 and 434°C. The products of the thermal decomposition were MgO and a spinel MgFe2O4. Experimentally it was found to be difficult to eliminate CO2 from inclusion in the interlayer during the synthesis of the iowaite compound and in this way the synthesised iowaite resembled the natural mineral.

Raman spectroscopy of the molybdate minerals chillagite (tungsteinian wulfenite-I4), stolzite, scheelite, wolframite and wulfenite

Raman spectra of chillagite, wulfenite, stolzite, scheelite and wolframite were obtained at 298 and 77 K using a Raman microprobe in combination with a thermal stage. Chillagite is a solid solution of wulfenite and stolzite. The spectra of these molybdate minerals are orientation dependent. The band at 695 cm-1 is interpreted as an antisymmetric bridging mode associated with the tungstate chain. The bands at 790 and 881 cm-1 are associated with the antisymmetric and symmetric Ag modes of terminal WO2 whereas the origin of the 806 cm-1 band remains unclear. The 4(Eg) band was absent for scheelite. The bands at 353 and 401 cm-1 are assigned as either deformation modes or as r(Bg) and (Ag) modes of terminal WO2. The band at 462 cm-1 has an equivalent band in the infrared at 455 cm-1 assigned as as(Au) of the (W2O4)n chain. The band at 508 cm-1 is assigned as sym(Bg) of the (W2O4)n chain.