Aerosol composition of urban and desert origin in the Eastern Mediterranean. I

Aerosol samples were collected in Tel-Aviv, Israel, during two different atmospheric situations, clear days and dust storms, and were analyzed for shape, size distribution, elemental composition, and presence of sulfate in individual particles. Results of two cases are presented in this paper. In both cases about 80% of the 0.2 to 2.0 µm particles contained sulfate. On the clear day over 50% of the total were pure sulfates while 27% were mixed sulfates; on the dusty day 63% were mixed sulfates — desert particles coated with sulfate — and only 20% were pure sulfates. The sulfate content of the desert particles was fairly high, on the order of 0.1 g sulfate g^?1 of desert particles. A possible explanation of this phenomenon may be heterogeneous nucleation of SO₂ on the surfaces of insoluble desert particles during their passage over the Mediterranean.     

Land degradation: socioeconomic and environmental causes and consequences in the eastern Mediterranean

Land degradation is a natural and socioeconomic cause–effect phenomenon that is widespread all over the world. This study investigated the socioeconomic factors and causes of land degradation (e.g. population growth and urbanization, poverty, overgrazing, pollution, biodiversity, erosion) in the eastern part of the Mediterranean region. The study revealed a significant land use change from agricultural and natural vegetation to urbanized areas due to the high population increase during the last ca. 80 years (51‐times the magnitude of the total built‐up area). The high poverty rate that exists in the area (57 per cent of the population can be classed as ‘poor’) has resulted in damaging environmental practices (overgrazing and intensive usage of natural plants); we found 83 per cent of the farmers admitted to the adoption of these practices. Poverty has also resulted in an inverse and significant correlation (at the 95 per cent confidence level) between holding size and the sale of land for urban uses. We also noted that 75 per cent of the smallholder farmers surveyed had sold their lands for immediate benefits to cope with poverty. This relation was affected by the education level of the farmers; we found a direct and significant (95 per cent confidence level) correlation existed between these factors. Overgrazing was practised by 70 per cent of the farmers and was found to be one of the most important environmental consequences of land use change (1600 ha have been transformed from natural grazing to built‐up (urban) in the study area). Socio‐economic induced land degradation demands efforts to improve farmer environmental awareness as well as environmental standards, laws and bylaws and the reduction of mismanagement of land. Copyright © 2010 John Wiley & Sons, Ltd.     

Botanical origin and chemical composition of Brazilian propolis

Brazilian propolis has been classified into 12 groups based on physicochemical characteristics: five in the southern Brazil group (group 3), one in the southeastern Brazil group (group 12), and six in the northeastern Brazil group (group 6). The plant origins of these groups were investigated using reversed-phase high-performance thin-layer chromatography (RPHPTLC), reversed-phase high-performance liquid chromatography (RPHPLC), and gas chromatography-mass spectrometry (GC-MS). It was concluded that the origins of propolis group 3, group 6, and group 12 are resins of the poplar tree, Hyptis divaricata, and Baccharis dracunculifolia, respectively.     

Mineralogical composition of the clay fraction in alluvial soils of eastern Georgia

The mineralogical composition of the clay fractions separated from alluvial soils in the valleys of the Kura and Iori rivers—the main rivers of eastern Georgia—has been studied. It is shown that alluvial soils are very diverse with respect to their physicochemical properties, particle-size distribution, and mineralogy. In comparison with zonal automorphic soils, the alluvial soils have a lower content of organic matter and a coarser texture. The diversity of mineral associations in them is larger than that in the zonal soils.     

Ionic composition of rainwater and atmospheric aerosols in Sardinia,southern Mediterranean

The ionic composition of 55 aerosol samples and 31 precipitation events collected in a coastal site in southern Sardinia (Capo Carbonara, 39°06 N; 09°31 E) were compared. The samples were collected during one year period (Oct'90/Oct'91) and showed high variability in composition according to meteorological conditions. Rain and soluble part of aerosol showed a strikingly similar ionic composition: most significant anions were chlorine and sulphate, and sodium is the principal cations, followed by magnesium and calcium. The acid events are associated with N-NW trajectories (anthropogenic influxes from N. Europe) with avg. pH=4.65, non sea salt (nss) Ca=60 eq/l and NO₃/_nssSO₄=0.6. Southern precipitations are influenced by Saharan dust alkaline effects, with avg. pH=6.75,_nssCa=271 eq/l and NO₃/_nssSO₄=0.4. Na/Cl ratio in rain is similar to sea water (0.87), whilst in aerosols there is a Cl loss (Na/Cl=1.10), probably due to reaction with nitric acid. Total fluxes of Ca, Mg, NO₃ and SO₄ were 104, 9, 64 and 113 g/cm², and wet deposition exceeded (65–90%) dry deposition. Scavenging ratios (SR) as defined by the equation:SR=[(Ci)rain/(Ci)air] ^*d, (d=1200g/m³) were calculated, using geometric means (Ci) of precipitation and aerosols collected concurrently during the period (a total of 23 samples). The SR values are Ca=3400, Cl=2400, Na, K, SO₄=1700, Mg=1000 and NO₃=750. These numbers could be useful to infer total fluxes by using simply rainwater ionic composition in Mediterranean semi-arid sites like Sardinia.     

Some impacts of urban waste landfills on Mediterranean soils

Seventy soil samples around and under urban waste landfills in central Spain were studied for 28 physical and chemical properties. In the unaffected surroundings of landfills there is always a higher proportion of coarse and fine gravel. Chlorides, sulphates and nitrates increase noticeably in all the soils affected by landfills as do Na⁺, B³⁺ and Zn²⁺. Multivariate analyses show that higher or lower water retention in the surface layer plays a main role in the organization of both acid and sandier soils as well as of basic soils and those with a higher proportion of silt and clay. Depending on the acidity or basicity, however, the other main factors reveal different hierarchical levels in the soil variables with regard to the organization of these systems. Thus, in acid soils, Zn²⁺ and B³⁺ contribute most noticeably to the second hierarchical level in the edaphic organization. In basic soil without gypsum, the second important gradient of variation is the stoniness (gravel)–fine sand (<2 mm fraction) while the importance of the K⁺, B³⁺ and SO₄⁼ is relegated to the third factor. In the basic soils with gypsum, not only sulphate, but also Na⁺, Cl⁻ and Zn²⁺ plays an essential role in the first factor and the coarse surface elements are also important. The principal components analysis made it possible to establish the main factors involved in the degradation caused by leachates from landfills. Consequently, greater attention could be given to these factors with a view to rehabilitation of degraded soils. © 1998 John Wiley & Sons, Ltd.     

Soil collembolan communities on north- and south-facing slopes of an eastern Mediterranean valley

The present paper includes the first comprehensive list of a collembolan community in a site in Israel. Comparison was made between the assemblage of collembolan species on the north- and south-facing slopes of Lower Nahal Oren, Mt. Carmel, Israel. The valley runs from east westward. Its slopes, only 100 m apart at the bottom, contrast sharply due to the much higher solar radiation on the south-facing slope. The assemblage of Collembola found includes 50 Arthropleona and 20 Symphypleona species, including 14 species that are new to science. Arthropleona species richness was very similar on the north slope (43) and the south-facing slope (41). In contrast, a rich assemblage of Symphypleona was recorded on the north-facing slope (19 species), but only eight were recorded on the south-facing slope. Differences in species richness were found between and within slopes according to altitude zone, soil depth and vegetation. Collembola of the alluvial zone on the contrasting slopes were more similar to each other than those of the alluvial zone on each slope with its adjacent altitudinal zone on the same slope.     

Dynamics of contamination of urban soils with lead in the eastern district of Moscow

Spatial-temporal trends were revealed in the contamination of Moscow soils with lead as a priority pollutant emitted with automobile exhaust. From the data of 1989 and 2005, maps of technogenic lead aureoles in soils of the eastern district were compiled, the average annual rate of increase in the element content was estimated, and its doubling time was predicted. Ecological-indication properties controlling the accumulation of lead in soils were determined.     

Lead isotope and trace element composition of urban soils in Mongolia

Lead (Pb) pollution in and around Ulaanbaatar is of national concern, given that the Mongolian capital is home to nearly half of the country’s entire population. By comparison, Mongolian countryside is a pristine environment because of its sparse population and low industrial activity. The concentration of Pb in urban soils (average of 39.1 mg kg^–1) was twice the values found (average 18.6 mg kg^–1) in background territories (i.e., Mongolian rural sites). Furthermore, Pb contamination was examined by using Pb stable isotopic composition, and covariance of Pb isotopic ratios showed two groups between rural and urban soils as pristine and disturbed sites. The ²⁰⁶Pb/²⁰⁷Pb ratio, the most prominent fingerprint for Pb pollution, was 1.163–1.185 for the urban whereas values for rural soils (1.186–1.207) were analogue to the regional Pb isotopic signatures. Local coal sources and their combustion products, one of the potential Pb pollution sources in Ulaanbaatar, have significant radiogenic properties in terms of Pb isotopic composition and revealed an average of 1.25 for ²⁰⁶Pb/²⁰⁷Pb and 19.551 for ²⁰⁶Pb/²⁰⁴Pb ratios. Thus, contributions from coal firing activity to Pb pollution lower than it was assumed, and smaller range of these values measured in urban soils may be attributed to the mixing of less radiogenic Pb as a constituent of the leaded gasolines.     

The use of urban organic wastes in the control of erosion in a semiarid Mediterranean soil

Abstract. A two year field experiment was carried out in a semiarid Mediterranean area in order to evaluate, the effect on soil erosion of adding different urban organic wastes: a stabilized municipal waste (compost), an unstabilized municipal waste, and an aerobic sewage sludge. All the treatments significantly reduced soil erosion, compared to the control soil. The soil amended with compost was the most effective treatment, reducing soil loss by 94% and runoff by 54%.     

Evolution, Sources and Distribution of Mineral Particles and Amorphous Phase of Atmospheric Aerosol in An Industrial and Mediterranean Coastal Area

The aim of this work is to propose a methodology that helps to learn about the distribution of different types of solid compounds in atmospheric aerosol, collected in an industrial area located in a Mediterranean basin that produces mineral raw materials. The work is developed from TSP samples collected daily in an open area near a ceramic production facility with a High Volume TSP sampler. The sampler permits the collection of sufficient daily quantities of particulate sample for subsequent X-ray diffraction characterisation and quantification. The results have shown that atmospheric aerosol in the area are dominated by particles coming from combustion processes, mainly vehicular traffic, and dust emissions originating when raw materials are transferred and treated. Combustion particles present a seasonal evolution. Mineral particles are mainly dependent upon weekly industrial activity and their contents suffer high increases during periods of atmospheric particle accumulation which are produced when certain meteorological conditions exist. Data have also shown an approximation of the particle distribution in aerosol from different source origins (vehicular traffic, dust emissions, secondary formation, marine aerosols). During days with intermediate pollution levels (which suppose 60% of the total) combustion particles compromise around 55 to 60% of the TSP while mineral particles coming from industrial dust emissions make up 20% of the TSP. In time intervals of atmospheric particulate accumulation these particle levels in the air can reach the legislated guideline values. During these episodes, mineral contents coming mainly from dust emissions compromise more than the 50% of the aerosol.     

Humic acid composition and humification processes in wetland soils of a Mediterranean semiarid wetland

Purpose

The present study focuses on a compositional characterization of the humic acid (HA) fraction of several wetland soils using solid-state ¹³C NMR spectroscopy. The data were analysed using the molecular mixing model (MMM), based on an empirical approach by Nelson and Baldock. The compositional data from HAs obtained with this model were used to obtain a wider assessment of the process of humification from comparison of total soil wetland organic matter composition and HA composition.

Materials and methods

Twenty samples of humic acids (HAs) isolated from a Mediterranean semiarid wetland (‘Tablas de Daimiel’, central Spain) were studied using elemental analysis and cross polarization magic angle spinning (CPMAS)¹³C nuclear magnetic resonance (NMR) spectroscopy. The NMR data were analysed with the molecular mixing model (MMM) considering up to six generic components (carbohydrate, protein, lignin, lipid, char and ‘carbonyl’). HAs are considered a conceptual mixture of these model components, and the MMM determines the proportions of the characteristic biomolecules contributing to HA composition.

Results and discussion

The composition of the HAs under study depends on local factors such as site vegetation and occurrence of fire. Correlations between the proportions of the six generic components and further comparison with those determined for the unfractionated OM (whole sample, WS), gave information on HA origin and humification mechanisms. In particular, the proportions of char and carbohydrate (R ² 0.637) and contents of lignin and protein (R ² 0.471) in the HAs were negatively correlated (P < 0.05). Significant correlations (R ² 0.439) also existed for char contents in whole sample (WS) compared to HA, and for carbohydrates in WS compared to HA (R ² 0.558). Char proportion grew in HA with respect to the WS, and carbohydrates dropped to a half on average in HA compared to WS.

Conclusions

Two different humification mechanisms could be identified for no-fire and fire areas. In the former, HA-char was preserved selectively from char in the sample, whereas in the latter, char was newly formed by fire effect.

     

Nematode community composition and diversity associated with a topoclimatic transect in a rain shadow desert

The effect of a topoclimatic gradient on soil nematode communities was investigated in the Israeli Judean Desert. Four locations along a 35 km gradient, from an elevation of 650 m above sea level with 620 mm rainfall to a –60 m relative to sea level with a rainfall below 110 m, were studied: Givat Yearim, Maale Adumim, Mishor Adumim and Kalia. Monthly soil samples were collected between January 1994 and December 1995. Thirteen nematode families and 17 genera were observed. Cephalobus, Heterocephalobus, Aphelenchoides, Tylenchus, Dorylaimus and Eudorylaimus were found to be the dominant genera. Ecological measurements of soil nematode community structure, diversity, and maturity indices were assessed, and comparisons between four locations and four seasons were made. Significant differences in the total numbers of nematodes were found between the locations (p < 0.01) and seasons (p < 0.05), where Givat Yearim > Maale Adumim > Mishor Adumim > Kalia, winter > spring > autumn > summer. Bacterivores were found to be the most abundant trophic group across locations and seasons, with a mean relative abundance of 55.0%. The densities of bacterivores, plant parasites and omnivores-predators during the winter season exhibited similar trends at all four locations, with Givat Yearim > Maale Adumim > Mishor Adumim > Kalia. None of the ecological indices were significantly different between locations. However, the maturity index (MI), trophic diversity (TD) and Simpson diversity (SI) exhibited significant differences between seasons.     

Analysis of the mineral composition of taro for determination of geographic origin

The mineral composition of taro ( Colocasia esculenta (L.) Schott) was analyzed to develop a method to distinguish taro produced in Japan and China. The concentrations of 15 elements (Al, Ca, Cl, Mg, Mn, Br, Co, Cr, Cs, Fe, K, Na, Rb, Sc, Zn) were assayed using instrumental neutron activation analysis. The concentrations of NO(3)(-), SO(4)(2-), H(2)PO(4)(-), Cl(-), malate, and oxalate were measured by ion chromatography. The mean concentrations of H(2)PO(4)(-), Co, Cr, and Na significantly differed (P < 0.01) between taro grown in Japan and that grown in China. Discriminant analysis was performed to identify the most efficient combination of elements and compounds to discriminate the taro geographic origin. The highest percentage of correct classification was achieved with a two-variable model including H(2)PO(4)(-) and Co (100% for Japanese, 93.75% for Chinese). Principal component analysis and cluster analysis using all of the assayed elements and compounds were also conducted to determine which elements significantly accounted for the variation of the taro mineral composition. We report on the potential of H(2)PO(4)(-) and Co concentrations to differentiate taro grown in China and Japan and discuss the sources of variability in the taro mineral composition of our samples.     

The impact of marine reserves on nekton diversity and community composition in subtropical eastern Australia

The effectiveness of marine reserve protection on the biodiversity of aquatic assemblages (i.e. nekton) in subtropical eastern Australia was examined within two small (<6 km²) marine reserves and four non-reserve areas. The two marine reserves, and their corresponding non-reserves, were located in different geographical locations within Moreton Bay (north and south) and sites were surveyed with multiple hauls of a seine net. Species richness, evenness, density and mean size of the inshore communities were compared between the reserves and non-reserves. No statistical significant difference was detected in species richness between the areas however species evenness was significantly lower in the only non-reserve site impacted by commercial net fishing. Mean size of nekton was found to be significantly greater in the marine reserves compared to non-reserves but no statistical significant difference was found in the density of nekton between the study sites. Multivariate analysis revealed differences in community composition, particularly between the geographical locations where areas were impacted by different types of fishing pressure (recreational v commercial). These results highlight the impact commercial fishing can have on entire nekton assemblages, not just on targeted species. Our study demonstrates that the small marine reserves in Moreton Bay are protecting marine biodiversity and are thus at least partially achieving their management objective (to enhance the zone’s marine biodiversity).     

Prey depletion caused by overfishing and the decline of marine megafauna in eastern Ionian Sea coastal waters (central Mediterranean)

Surveys primarily aimed at determining dolphin encounter rates were conducted from small inflatable craft in eastern Ionian Sea coastal waters between 1997 and 2004. During 633 surveys totalling 21,276 km of effort, observations of cetaceans and other marine species spotted in a study area of 480 km² were systematically recorded. Common dolphin encounter rates declined 25-fold across the study period, steadily decreasing from 2.18 encounters/100 km in 1997 to 0.09 encounters/100 km in 2004. Encounter rates of tuna also declined significantly. Swordfish encounter rates dropped from 1.03 encounters/100 km in 1997 to 0-0.12 in 1998-2004. Encounter rates of bottlenose dolphins did not show significant trends. The decline of high-order marine predators feeding on epipelagic prey was consistent with the hypothesis of prey depletion, likely resulting from intensive exploitation of local fish stocks, particularly anchovies and sardines. The catholic feeding habits and opportunistic behaviour of bottlenose dolphins may allow them to withstand the effects of overfishing at their present low density.     

Near-infrared spectroscopy in saffron quality control: determination of chemical composition and geographical origin

Near-infrared reflectance spectroscopy has been applied for the first time to saffron spice to determine the chemical composition and geographical origin of 111 samples from the there main producers' countries: Iran, Greece, and Spain. The validation procedures with the results obtained by UV-vis and HPLC-DAD measurements demonstrated that this technique is appropriate to determine the following parameters: moisture and volatile content, coloring strength, (250 nm), and (330 nm), established on the ISO 3632 Technical Specification Normative and used to certify saffron quality in the international market. Also, it can be used to estimate the content of the five main crocetin glycosides, the compounds responsible for saffron color, the best correlations being for trans-crocetin di-(beta-D-gentibiosyl) ester (R2= 0.93), trans-crocetin (beta-D-glucosyl)-(beta-D-gentibiosyl) (R2= 0.94), and picrocrocin (R2= 0.92), the compound accepted as responsible for saffron bitterness. Finally, a discriminant analysis among the three geographical origins reveals that Iranian samples are the most different, whereas Greek and Spanish samples are more similar. All of these results reveal that NIRS spectroscopy has an enormous potential for its application to saffron quality control as the results are obtained in 2 min and without any sample manipulation.     

Edaphic characterization and soil ionic composition influencing plant zonation in a semiarid Mediterranean salt marsh

Soil characteristics and plant zonation were studied in a semiarid Mediterranean salt marsh in SE Spain. According to topographic sequences and plants distribution, two transects were established from the border of La Mata lagoon to the upland vegetation limit and soils were described and analysed. Regularly spaced plots were established in these transects in accordance with the stands of vegetation and surface soil samples were taken every 2 months for 2 years. The following edaphic factors were determined: soil moisture content, pH and concentration of Cl⁻, SO₄²⁻, Ca²⁺, Mg²⁺, Na⁺ and K⁺ in the saturation extract. In addition, the groundwater level was measured and the duration of the flooding periods established in each plot. Soil–plant relationships were studied by means of canonical correspondence analysis. Based on rainfall data for the study period, dry and wet seasons were separated and the habitats of the plant communities were compared for salt quantity and quality independently for each season. Soils were classified, according to FAO (1998), as Hypercalcic, Sodic and Mollic Solonchaks and Hypercalcic Sodic Calcisols. The most important variables which explained plant zonation were: the flooding period, total salinity, minimum Ca²⁺/Na⁺ ratio and the mean sodium adsorption ratio. When the habitats of the main plant communities were compared, differences in salt quantity, quality and seasonal variations were found. Two chenopod shrubs, Arthrocnemum macrostachyum and Sarcocornia fruticosa, predominated in the most saline areas. More pronounced seasonal variations in soil salinity were found in the A. macrostachyum zone than in the Sarcocornia fruticosa zone. The highest value for K⁺/Na⁺ and Ca²⁺/Na⁺ ratios were measured in the Suaeda vera stand. The Lygeum spartum zone was distinguished by the high Ca²⁺/Na⁺ and Ca²⁺/Mg²⁺ ratios in the wet period. Among the rushes, Schoenus nigricans predominated in the less saline areas, where the K⁺/Na⁺ ratio was higher and the Ca²⁺/Na⁺ ratio lower than where Juncus maritimus predominated. Limonium cossonianum communities occupied an intermediate position with respect to soil salinity, between the chenopod shrubs and the other communities.Our results suggest that salt marsh plant zonation is influenced by temporal and spatial edaphic gradients which must be jointly considered if soil–plant relationships in saline soils are to be fully understood.