Humic acid (HA) is well known as an inexpensive and effective adsorbent for heavy metal ions. However, the thermodynamics of uranium (U) adsorption onto HA is not fully understood. This study aimed to understand the kinetics and isotherms of U(VI) adsorption onto HA under different temperatures from acidic water. A leonardite-derived HA was characterized for its ash content, elemental compositions, and acidic functional groups, and used for the removal of U (VI) from acidic aqueous solutions via batch experiments at initial concentrations of 0–100 mg·L⁻¹ at 298, 308 and 318 K. ICP-MS was used to determine the U(VI) concentrations in solutions before and after reacting with the HA. The rate and capacity of HA adsorbing U(VI) increased with the temperature. Adsorption kinetic data was best fitted to the pseudo second-order model. This, together with FTIR spectra, indicated a chemisorption of U(VI) by HA. Equilibrium adsorption data was best fitted to the Langmuir and Temkin models. Thermodynamic parameters such as equilibrium constant (K₀), standard Gibbs free energy (ΔG⁰), standard enthalpy change (ΔH⁰), and standard entropy change (ΔS⁰), indicated that U(VI) adsorption onto HA was endothermic and spontaneous. The co-existence of cations (Cu²⁺, Co²⁺, Cd²⁺ and Pb²⁺) and anions (HPO₄²⁻ and SO₄²⁻) reduced U(VI) adsorption. The high propensity and capacity of leonardite-derived HA adsorbing U(VI) suggests that it has the potential for cost-effective removal of U(VI) from acidic contaminated waters.

This study aimed to investigate the effects of r-type exopolysaccharides (EPSs) produced by the symbiotic bacteria Rhizobium tropici on soil aggregate formation and stability in loess sandy soil and to elucidate the independent and synergistic roles of EPSs in soil structure development. Experiments were conducted under both sterile and non-sterile soil conditions to distinguish the direct effects of EPSs from their interactions with indigenous soil microorganisms. Soil samples were treated with varying concentrations of EPSs and compared with untreated controls after undergoing a simulated weathering process. Aggregates were classified into four size fractions: 53 μm), with approximately 80% increases in the number of aggregates in the 53–250 μm and 2000–5000 μm fractions compared to the control. Soil stability was markedly enhanced, with a 41.7% increase in >0.25 mm water-stable aggregates, a 36.4% rise in MWD, and a 0.3% increase in GMD. The D decreased by 1.2% under 0.2‰ EPS treatment, indicating a more ordered soil structure. EPSs play a key role in promoting soil aggregate formation and enhancing soil stability. While microbial presence has a limited short-term effect on aggregation, the synergistic interaction between microorganisms and EPSs over time significantly enhances soil stability. This study provides new insights into understanding the independent and synergistic roles of EPSs in soil structure formation.

This study investigated the effects of exopolysaccharide (EPS) addition on the formation and stability of water-stable aggregates in rhizosphere and bulk soils. A pot experiment was conducted using soils treated with EPS concentrations of 0.00‰, 0.25‰, 0.50‰, and 1.00‰. Soil aggregates were fractionated into four fractions, namely >2000 μm, 250–2000 μm, 53–250 μm, and 2000 μm and 250–2000 μm) while reducing smaller particles (2000 μm and 250–2000 μm) were positively correlated with each other but showed weak or non-significant relationships with plant biomass parameters. In particular, the 250–2000 μm fraction exhibited a weak negative correlation with total biomass (r = −0.37, p ≤ 0.05). These findings highlight the potential of moderate EPS concentrations to enhance soil structure and stability, particularly in rhizosphere soils, providing insights into its application for sustainable soil management.