EUSA Review 21/2 Spring 2008

No abstract.

EUSA Review 22/2 Spring 2009

No abstract.

EUSA Review 22/3 Spring 2009

No abstract.

EUSA Review 23/2 Spring 2010

No abstract.

EUSA Review 24/2 Spring 2011

No abstract.

EUSA Review 26/2 Spring 2013

No abstract.

EUSA Review 27/1 Spring 2014 [last volume in series]

No abstract.

The socio-economic of exclusion: Re-questioning citizenship in relation to social justice in the post Arab Spring Egypt. Arab Citizenship Review No. 15, 19 February 2016

The most recent official statistics reveal that over a quarter of Egypt’s population still live in poverty, a third of its youth are unemployed and three out of five children are malnourished. Much of the criticism of Egypt’s human rights record, particularly after the Arab Spring, remains focused on the country’s civil and political rights, and freedoms with an intentional (or unintentional) disregard to socioeconomic rights, fuelling widespread poverty, deteriorating living standards, socioeconomic exclusion and unequal and/or degrading treatment. This paper examines the socioeconomic policies of exclusion that are still undermining the enjoyment of basic citizenship rights in Egypt.

Fossil and non-fossil source contributions to atmospheric carbonaceous aerosols during extreme spring grassland fires in Eastern Europe

In early spring the Baltic region is frequently affected by high-pollution events due to biomass burning in that area. Here we present a comprehensive study to investigate the impact of biomass/grass burning (BB) on the evolution and composition of aerosol in Preila, Lithuania, during springtime open fires. Non-refractory submicron particulate matter (NR-PM1) was measured by an Aerodyne aerosol chemical speciation monitor (ACSM) and a source apportionment with the multilinear engine (ME-2) running the positive matrix factorization (PMF) model was applied to the organic aerosol fraction to investigate the impact of biomass/grass burning. Satellite observations over regions of biomass burning activity supported the results and identification of air mass transport to the area of investigation. Sharp increases in biomass burning tracers, such as levoglucosan up to 683 ngm-3 and black carbon (BC) up to 17 μgm-3 were observed during this period. A further separation between fossil and non-fossil primary and secondary contributions was obtained by coupling ACSM PMF results and radiocarbon (14C) measurements of the elemental (EC) and organic (OC) carbon fractions. Non-fossil organic carbon (OCnf/ was the dominant fraction of PM1, with the primary (POCnf/ and secondary (SOCnf/ fractions contributing 26–44% and 13–23% to the total carbon (TC), respectively. 5–8% of the TC had a primary fossil origin (POCf/, whereas the contribution of fossil secondary organic carbon (SOCf/ was 4–13 %. Nonfossil EC (ECnf/ and fossil EC (ECf/ ranged from 13–24 and 7–13 %, respectively. Isotope ratios of stable carbon and nitrogen isotopes were used to distinguish aerosol particles associated with solid and liquid fossil fuel burning.