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High silica zeolite Y has been positively evaluated to clean-up water polluted with sulfonamides, an antibiotic family which is known to be involved in the antibiotic resistance evolution. To define possible strategies for the exhausted zeolite regeneration, the efficacy of some chemico-physical treatments on the zeolite loaded with four different sulfonamides was evaluated. The evolution of photolysis, Fenton-like reaction, thermal treatments, and solvent extractions and the occurrence in the zeolite pores of organic residues eventually entrapped was elucidated by a combined thermogravimetric (TGA-DTA), diffractometric (XRPD), and spectroscopic (FT-IR) approach. The chemical processes were not able to remove the organic guest from zeolite pores and a limited transformation on embedded molecules was observed. On the contrary, both thermal treatment and solvent extraction succeeded in the regeneration of the zeolite loaded from deionized and natural fresh water. The recyclability of regenerated zeolite was evaluated over several adsorption/regeneration cycles, due to the treatment efficacy and its stability as well as the ability to regain the structural features of the unloaded material.

Humic acids (HAs) extracted from soils developed under two Norwegian spruce (Picea abies, (L.) Karst) subalpine forests of northern Italy were characterized using chemical, thermal (TG-DTA) and spectroscopic (DRIFT) analyses. The samples were taken from five sites which differed in orientation (northern and southern exposure) and vegetal cover at different old age: grassland, regeneration, immature and mature stands. In general, the thermal patterns of HAs were similar (three exothermic reactions appeared around at 300, 400 and 500°C) in both sites in grasslands and regeneration while a considerable modification appeared in HA from stands of different age at northern and southern exposure site. DRIFT spectroscopy confirmed the differences observed through TG-DTA analysis. In particular the main structural changes were ascribed to modification of carbonyl group and of CH stretching in aliphatic components in each HAs from different sites

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Although acid soils are common in forest ecosystems, and there is documented evidence of pH influencing transformations of organic matter in soil, there are surprisingly few studies on the influence of soil pH on the chemical structure of physically fractionated soil organic matter (SOM). The aim of this study was to characterize the influence of pH on the chemical and physical processes involved in SOM stabilization. Forest soils of different pH (4.4 and 7.8) sampled from two long‐term experiments at Rothamsted Research (UK) were physically fractionated. The free light fraction (FLF), the intra‐aggregate light fraction and the fine silt and clay (S + C, <25 µm) were characterized using elemental, isotopic (δ13C), thermogravimetric, differential thermal, diffuse reflectance infrared Fourier transform spectroscopy and high‐resolution magic angle spinning 1H nuclear magnetic resonance analyses. The quantitative distribution of carbon (C) between SOM fractions differed between the two soils. Carbon contents in the light fractions from the acid soil were significantly greater than in those of the alkaline soil. In contrast, in S + C fractions, C content was greater in the alkaline soil. FLF from the acid soil was characterized by a greater C:N ratio, smaller δ13C and greater content of thermo‐labile compounds compared with FLF from the alkaline soil. In contrast, there was only a weak effect of soil pH on the chemical composition of the organic matter in S + C fractions. Irrespective of soil pH, these latter fractions contained mainly aliphatic compounds such as carbohydrates, carboxylic acid, amide and peptide derivates. This suggested that physical mechanisms, involving the interactions between SOM and mineral surfaces, are of greater importance than the presence of chemically recalcitrant species in protecting SOM associated with the finest soil fractions.