The influence of marine environment on the conservation state of Built Heritage: An overview study

Marine aerosol is a chemical complex system formed by inorganic salts and organic matter, together with airborne particulate matter from the surrounding environment. The primary particles transported in the marine aerosol can experiment different chemical reactions in the atmosphere, promoting the so-called Secondary Marine Aerosol particles. These kinds of particles (nitrates, sulfates, chlorides etc.), together with the natural crustal or mineral particles and the metallic airborne particulate matter emitted by anthropogenic sources (road traffic, industry, etc.) form clusters which then can be deposited on building materials from a specific construction following dry deposition processes. Apart from that, the acid aerosols (e.g. CO₂, SO₂, NO_X, etc.) present in urban-industrial environments, coming also from anthropogenic sources, can be deposited in the buildings following dry or a wet deposition mechanisms. The interactions of these natural and anthropogenic stressors with building materials can promote different kind of pathologies. In this overview, the negative influence of different marine environments (direct or diffuse influence), with or without the influence of an urban-industrial area (direct or diffuse), on the conservation state of historical constructions including a wide variety of building materials (sandstones, limestones, artificial stones, bricks, plasters, cementitious materials, etc.) is presented.

Micro-Raman and SEM-EDS analyses to evaluate the nature of salt clusters present in secondary marine aerosol

Marine aerosol is a complex inorganic and organic chemistry system which contains several salts, mainly forming different type of salt clusters. Different meteorological parameters have a key role in the formation of these aggregates. The relative humidity (%RH), temperature, CO, SO₂ and NO_x levels and even the O₃ levels can promote different chemical reactions giving rise to salt clusters with different morphology and sizes. Sulfates, nitrates and chlorides and even mixed chlorosulfates or nitrosulfates are the final compounds which can be found in environments with a direct influence of marine aerosol. In order to collect and analyze these types of compounds, the use of adequate samplers is crucial. In this work, salt clusters were collected thanks to the use of a self-made passive sampler (SMPS) installed in a 20th century historic building (Punta Begoña Galleries, Getxo, Basque Country, Spain) which is surrounded by a beach and a sportive port. These salt clusters were finally analyzed directly by micro-Raman spectroscopy and Scanning Electron microscopy coupled to Energy Dispersive X-ray spectrometry (SEM-EDS).

Statistical evaluation of aerosol data from Ben Macdhui mountain, South Africa

The aim of this study is re-evaluation of the data collected during Ben Macdhui High Altitude Trace Gas and Aerosols Transport Experiment (BHATTEX) to identify the dominant species of aerosols and their interactions in the atmosphere. Particularly, investigations of seasonal variations, the origin of sulphates and the formation of the ammonia sulphate were essential topics of this study. Such analyses were done by application of unique combination of supervised and unsupervised learning classification methods. Namely discriminant function analysis (DFA) for simple identification of parameters and principal component analysis (PCA) for the further investigations on hidden structure of data has been applied. The analysis shows that sulphate concentration and C,N isotopic ratios can classify winter and summer patterns of data. Differences between sulphate concentrations in summer and winter samples indicated by second PCA component were probably related to meteorological conditions over that region. The relations between anthropogenic compounds and ammonia or sulphate were much more stronger in summer samples than in winter ones, that is related with seasonal transport of that particles from industry to the investigated regions. The hypothesis of competitive reaction between sulphates, nitrates and ammonia ions has been also proven by application of simple regression analysis. Moreover the analysis of correlations coefficients shows that those relations are independent on seasons.

Marine aerosol production: a review of the current knowledge

The current knowledge in primary and secondary marine aerosol formation is reviewed. For primary marine aerosol source functions, recent source functions have demonstrated a significant flux of submicrometre particles down to radii of 20 nm. Moreover, the source functions derived from different techniques up to 10 microm have come within a factor of two of each other. For secondary marine aerosol formation, recent advances have identified iodine oxides and isoprene oxidation products, in addition to sulphuric acid, as contributing to formation and growth, although the exact roles remains to be determined. While a multistep process seems to be required, isoprene oxidation products are more likely to participate in growth and sulphuric acid is more likely to participate in nucleation. Iodine oxides are likely to participate in both nucleation and growth.