Formation of Organic Sulfur Compounds through SO₂ Initiated Photochemistry of PAHs and DMSO at the Air-Water Interface

The presence of organic sulfur compounds (OSs) at the water surface, acting as organic surfactants, may influence the air-water interaction and contribute to new particle formation in the atmosphere. However, the impact of ubiquitous anthropogenic pollutant emissions, such as SO2 and polycyclic aromatic hydrocarbons (PAHs) on the formation of OSs at the air-water interface still remains unknown. Here, we observe large amounts of OSs formation in presence of SO2, upon irradiation of aqueous solutions containing typical PAHs such as pyrene (PYR), fluoranthene (FLA), and phenanthrene (PHE), as well as dimethylsulfoxide (DMSO). We observe rapid formation of several gaseous OSs from light-induced heterogeneous reactions of SO2 with either DMSO or a mixture of PAHs/DMSO, and some of these OSs (e.g. methanesulfonic acid) are well established secondary organic aerosol (SOA) precursors. A myriad of OSs and unsaturated compounds are produced and detected in the aqueous phase. The tentative reaction pathways are supported by theoretical calculations of the reaction Gibbs energies. Our findings provide new insights into potential sources and formation pathways of OSs occurring at the water (sea, lake, river) surface, that should be considered in future model studies to better represent the air-water interaction and SOA formation processes.

Improving the stability of beech wood with polyester treatment based on malic acid

The improvement of durability and dimensional stability of wood properties via modification of the microstructure and wood–water interaction has been widely utilised. This study investigated polyester treatments, a possible alternative, using environmentally friendly chemicals such as malic acid to improve the beech wood (Fagus sylvatica) properties. The modified properties have been studied with four treatments using malic acid, glycerol, butanediol and succinic anhydride, mixing polycarboxylic acids and polyols. Results showed that the anti-swelling-efficiency (ASE) improved up to 70%, and the bulking coefficient improved around 23%, exhibiting an efficient penetration within the cell walls. The leaching rates (LR) of treatments and the extractables remained low, between 0.05 and 2.4%. The equilibrium moisture content (EMC) decreased by 50% for the four treatments, compared to untreated beech wood.

Wind-Wave Interaction in Sengguruh Reservoir and The Effect to Riprap Material

The Sengguruh Dam is one of the large dams managed by Jasa Tirta I Public Company. This reservoir has been operating for more than 38 years (operating since 1982 and the latest data is for 2020). This research was conducted to determine the effect of wind and the interaction of wind on the water in the Sengguruh Dam. Most of the interaction of water and wind is mostly carried out on coastal structures but rarely investigated in the upstream area of the river basin. Investigations were carried out to obtain an overview and characteristics of the influence of the two variables of wind and water on the hydraulics of the reservoir storage, sedimentation in the water column, and side effects of the embankment material in the riprap dam. This study will provide an overview of the condition of the Sengguruh Dam which is full of sediment and shows the wind and water interaction that occurs in the reservoir as well as the potential hazards that are quite large for the management of water resources and disasters in the surrounding community if there is a high risk or threat that occurs if these conditions do not meet dam safety standards in Indonesia.

Durability of UHPFRC functionalised with nanoadditives due to synergies in the action of sulphate and chloride in cracked and uncracked states

This paper studies the durability of Ultra High Performance Fibre Reinforced Concrete (UHPFRC) with high Blast Furnace Slag content (BFS) and nanoadditives such as crystalline admixture (CA), alumina nanofibres (ANF) and cellulose nanocrystals (CNC), exposed to different aggressive environmental conditions: 1) three aggressive media: a) deionized water (dw), b) sulphate rich solution (ss) and c) simulated geothermal water (sgw) containing sulphate and chloride; 2) two water interaction conditions: a) static and b) dynamic (water impact); and 3) with and without the presence of cracks. Durability was analysed over 24 months, measuring several physical and chemical parameters of the system, recording changes in both the aggressive media and the concrete. All UHPFRC types demonstrate good durability, showing high resistance to expansion and deformation in the sulphate-rich media. A leaching process occurs in all water interaction systems, the dynamic interaction in sgw being the most aggressive. The interaction of sgw inside the crack favours the formation of solid phases such as calcium carbonates and ettringite, while the presence of nanoadditives affects the response of both the matrix and the formation of precipitates within the crack.

Groundwater and Surface Water Interaction, Wairarapa Valley, New Zealand

<p>Physical and chemical interactions between surface and groundwater are complex and display significant spatial and temporal variability. However, relatively little is known about the chemical interaction between surface and groundwater; in particular the temporal scales at which this interaction occurs. The aim of this research was to determine if existing and/or potential water chemistry measurements could be used to investigate the interaction between surface and groundwater bodies in the Wairarapa valley, New Zealand and identify specific locations and timescales at which this interaction occurs. Analyses were undertaken at both regional and local scales. The regional scale investigation utilised Hierarchical Cluster Analysis (HCA) to categorise 268 historic surface and groundwater sites from the 3000 km² Wairarapa valley into similar hydrochemical clusters in order to infer potential interaction. Six main clusters were identified, primarily differentiated by their total dissolved solids (TDS), redox potential and major ion ratios. Shallow aquifers, located in close proximity to losing reaches of the upper Ruamahanga, Waiopoua and Waiohine Rivers, were grouped with similar Ca²⁺-HCO₃⁻ type surface waters, indicating (potential) recharge from these river systems. Likewise, rainfall-recharged groundwater sites that displayed higher Na⁺ relative to Ca²⁺ and Cl⁻ relative to HCO₃⁻ were grouped with similar surface waters such as the Mangatarere and lower Waingawa streams. This suggests the provision of this rainfall-recharged signature to river base flow. Deep anoxic aquifers, high in TDS, were grouped together, but showed no statistical link to surface water sites. Results from the regional scale investigation highlight the potential use of HCA as a rapid and cost-effective method of identifying areas of surface and groundwater interaction using existing datasets. A local scale investigation utilised existing quarterly and monthly hydrochemical data from the Mangatarere and Waiohine Rivers and nearby groundwater wells in an attempt to gain insight into temporal variability in surface and groundwater interactions. Time series analysis and HCA were employed, however, the coarse time scales at which data was available made it difficult to make reliable inferences regarding this interaction. To overcome this issue, upstream and downstream surface and groundwater gauging stations were established in the Mangatarere Stream catchment for a 92 day period. Continuous electrical conductivity, water temperature and stage measurements were obtained at three of the four stations, along with one week of hydrochemical grab sampling. The fourth gauging station provided a more limited dataset due to technical issues. The downstream Mangatarere Stream received 30-60% of base flow from neighbouring groundwaters which provided cool Na⁺-Cl⁻ type waters, high in TDS and NO₃‾ concentrations. This reach also lost water to underlying groundwaters during an extended dry period when precipitation and regional groundwater stage was low. The upstream groundwater station received recharge primarily from precipitation as indicated by a Na⁺-Cl⁻-NO₃‾ signature, the result of precipitation passage through the soil-water zone. However, it appeared 2-4 m³/s of river recharge was also provided to the upstream groundwater station by the Mangatarere stream during an extended storm event on JD021-028. Mangatarere surface waters transferred a diurnal water temperature pattern and dilute Na⁺-Ca²⁺-Mg²⁺-HCO₃⁻-Cl⁻ signature to the upstream groundwater station on JD026-028. Results obtained from the Mangatarere catchment confirm the temporal complexities of ground and surface water interaction and highlight the importance of meteorological processes in influencing this interaction.</p>

Groundwater and Surface Water Interaction, Wairarapa Valley, New Zealand

<p>Physical and chemical interactions between surface and groundwater are complex and display significant spatial and temporal variability. However, relatively little is known about the chemical interaction between surface and groundwater; in particular the temporal scales at which this interaction occurs. The aim of this research was to determine if existing and/or potential water chemistry measurements could be used to investigate the interaction between surface and groundwater bodies in the Wairarapa valley, New Zealand and identify specific locations and timescales at which this interaction occurs. Analyses were undertaken at both regional and local scales. The regional scale investigation utilised Hierarchical Cluster Analysis (HCA) to categorise 268 historic surface and groundwater sites from the 3000 km² Wairarapa valley into similar hydrochemical clusters in order to infer potential interaction. Six main clusters were identified, primarily differentiated by their total dissolved solids (TDS), redox potential and major ion ratios. Shallow aquifers, located in close proximity to losing reaches of the upper Ruamahanga, Waiopoua and Waiohine Rivers, were grouped with similar Ca²⁺-HCO₃⁻ type surface waters, indicating (potential) recharge from these river systems. Likewise, rainfall-recharged groundwater sites that displayed higher Na⁺ relative to Ca²⁺ and Cl⁻ relative to HCO₃⁻ were grouped with similar surface waters such as the Mangatarere and lower Waingawa streams. This suggests the provision of this rainfall-recharged signature to river base flow. Deep anoxic aquifers, high in TDS, were grouped together, but showed no statistical link to surface water sites. Results from the regional scale investigation highlight the potential use of HCA as a rapid and cost-effective method of identifying areas of surface and groundwater interaction using existing datasets. A local scale investigation utilised existing quarterly and monthly hydrochemical data from the Mangatarere and Waiohine Rivers and nearby groundwater wells in an attempt to gain insight into temporal variability in surface and groundwater interactions. Time series analysis and HCA were employed, however, the coarse time scales at which data was available made it difficult to make reliable inferences regarding this interaction. To overcome this issue, upstream and downstream surface and groundwater gauging stations were established in the Mangatarere Stream catchment for a 92 day period. Continuous electrical conductivity, water temperature and stage measurements were obtained at three of the four stations, along with one week of hydrochemical grab sampling. The fourth gauging station provided a more limited dataset due to technical issues. The downstream Mangatarere Stream received 30-60% of base flow from neighbouring groundwaters which provided cool Na⁺-Cl⁻ type waters, high in TDS and NO₃‾ concentrations. This reach also lost water to underlying groundwaters during an extended dry period when precipitation and regional groundwater stage was low. The upstream groundwater station received recharge primarily from precipitation as indicated by a Na⁺-Cl⁻-NO₃‾ signature, the result of precipitation passage through the soil-water zone. However, it appeared 2-4 m³/s of river recharge was also provided to the upstream groundwater station by the Mangatarere stream during an extended storm event on JD021-028. Mangatarere surface waters transferred a diurnal water temperature pattern and dilute Na⁺-Ca²⁺-Mg²⁺-HCO₃⁻-Cl⁻ signature to the upstream groundwater station on JD026-028. Results obtained from the Mangatarere catchment confirm the temporal complexities of ground and surface water interaction and highlight the importance of meteorological processes in influencing this interaction.</p>