The research, led by Kunyu Si and corresponding author Shuya Hu of Qingdao University, together with colleagues from the Yellow Sea Fisheries Research Institute, Hebei GEO University, and other institutions, focused on sediments collected from the Bailang River estuary on the southern shore of Laizhou Bay. Estuaries are notoriously complex geochemical reactors: where freshwater rivers meet the sea, salinity, pH, dissolved organic matter, and ionic strength can change dramatically over short distances. Earlier work on BTEX behavior had concentrated on inland soil–groundwater systems, leaving the brackish transition zones largely unexplored. The team chose the Bailang River site precisely because it exemplifies these sharp freshwater–seawater interactions, and because BTEX pollution from petrochemical, industrial, and transport activities is a persistent threat to shallow groundwater in such regions.

The experimental approach was elegantly simple but rigorous: one-dimensional dynamic column experiments in the laboratory. Ten identical organic glass columns, 15 centimeters tall and 3 centimeters in diameter, were packed from the bottom up with a quartz sand layer, 12 centimeters of sieved estuarine sediment, a 1-centimeter layer of artificially BTEX-contaminated soil, and a final protective sand cap. The contaminated layer was prepared by spraying a BTEX standard solution—prepared at 20 times the concentrations observed in the Laizhou Bay estuary—onto 1,000 grams of ground soil, which was then sealed to prevent volatilization. Leaching solutions of controlled chemistry were supplied from a constant-head tank and allowed to percolate downward by gravity under fully saturated conditions.

The hydrological parameters were carefully quantified. Based on local rainfall in Weifang City and the column’s 7.07-square-centimeter cross-section, the researchers calculated a total leaching volume of 400 milliliters per run. The measured average infiltration rate was 0.42 milliliters per minute, corresponding to a Darcy velocity of roughly 0.059 centimeters per minute. With a 12-centimeter soil column, a 5-centimeter water head, and a total head difference of 17 centimeters, the hydraulic gradient was approximately 1.42. Each leaching run lasted about 16 hours, after which the column was allowed to rest for two hours before being dismantled. Soil was sampled in three layers—0 to 4, 4 to 8, and 8 to 12 centimeters—then freeze-dried and extracted ultrasonically in chromatographic-grade methanol for analysis by gas chromatography–mass spectrometry using an Agilent 7890B-5977A instrument with a DB-5MS capillary column and selected ion monitoring. Method detection limits for the nine target compounds ranged from 0.05 to 0.12 micrograms per kilogram, spiked recoveries fell between 82.6 and 106.4 percent, and calibration correlation coefficients exceeded 0.995, satisfying USEPA method 8260D quality requirements.

The first major finding concerned acidity. When leaching solutions of pH 4, 7, and 11 were compared, neutral conditions proved most favorable for BTEX migration, with overall transport following the order neutral greater than alkaline greater than acidic. In the 0-to-4-centimeter layer—the zone of most intense movement—toluene migrated furthest, with ortho-xylene and ethylbenzene also showing high mobility. The mechanistic explanation lies in the behavior of humic acid, the dominant organic macromolecule in the sediment. Under acidic conditions, abundant hydrogen ions protonate the carboxyl and phenolic hydroxyl groups on humic acid, causing the coiled, contracted molecules to become more hydrophobic and exposing additional hydrophobic binding sites. Because BTEX are hydrophobic organic compounds that preferentially partition into such nonpolar microdomains, this contraction effectively locks them in place. Under alkaline conditions, the opposite occurs: extensive deprotonation extends the organic chains into dispersed nanoscale colloids that can either ferry adsorbed BTEX downward with the flow or clog pore throats—two competing effects that leave alkaline migration intermediate between neutral and acidic. At pH 7, colloids sit near their point of zero charge, the organo-mineral structure stays loose, and BTEX move freely as dissolved solutes driven by advection and dispersion.

The second factor, organic matter content, told a more straightforward story. As expected from partitioning theory, increasing organic matter significantly enhanced the medium’s adsorption and retention capacity, so migration amounts followed the order low, then medium, then high organic content. Humic substances contain abundant nanoscale hydrophobic microdomains built from aliphatic chains and aromatic rings, and BTEX molecules “escape” the polar aqueous phase into these compartments—a linear, reversible partitioning process that produces slow desorption tailing under continuous leaching. Interestingly, 1,2,4-trimethylbenzene showed the highest migration in the top layer under low-organic conditions, at roughly 22 nanograms per gram, while benzene dropped to just 7.33 nanograms per gram. The authors note that such compound-specific differences reflect an interplay of hydrophobicity, adsorption, and biodegradability: simple molecules like benzene and toluene are readily degraded by microbes, whereas heavily methyl-substituted compounds resist biodegradation thanks to steric hindrance and ring stabilization. The added humic acid may also have fueled heterotrophic microbial activity, although the study did not directly measure microbial parameters, so this remains a hypothesis for future testing.

Salinity emerged as a powerful brake on downward migration. Under pure water, low-salinity artificial seawater (S = 10), and high-salinity seawater (S = 30), migration amounts followed a clear descending order. The underlying physics is classic colloid chemistry. According to DLVO theory, the low ionic strength of pure water maintains a thick electrical double layer on the surfaces of clay minerals and organic colloids—long Debye lengths, high absolute zeta potentials typically exceeding 30 millivolts—keeping particles dispersed and stable. Hydrophobic BTEX compounds such as toluene, ethylbenzene, and o-xylene readily partition onto these mobile nanoscale carriers, riding them downward in so-called colloid-facilitated transport. As salinity rises, the diffuse double layer compresses, electrostatic repulsion weakens, colloids aggregate and settle, and the population of mobile carriers collapses. Simultaneously, the salting-out effect lowers the apparent aqueous solubility of the hydrocarbons, pushing them from dissolved to solid-adsorbed states. The surface 0-to-4-centimeter layer retained roughly twice the pollutant mass of the deeper 4-to-12-centimeter zone, confirming that the topmost sediment is the principal battleground.

The nutrient experiments added a final twist. Adding potassium nitrate to the leaching solution—an intervention relevant because nitrate can serve as an electron acceptor for anaerobic biodegradation of BTEX—suppressed migration compared with pure water. In the 0-to-4-centimeter layer, migration under pure water was about 50 percent higher than under nitrate treatment; at 4 to 8 centimeters the gap narrowed to roughly 33 percent, and at 8 to 12 centimeters the difference nearly vanished. Benzene, the most soluble and smallest of the nine compounds, was almost undetectable below the surface layer under nitrate leaching, appearing only in the top layer at 4.43 nanograms per gram—about one quarter of its pure-water value. The explanation combines two effects: dissolved potassium nitrate raises ionic strength, triggering salting-out and double-layer compression by potassium ions, while nitrate may simultaneously fuel nitrate-reducing biodegradation in the sediment. The authors caution that because redox potential, microbial activity, and nitrate transformation were not directly monitored, the relative contributions of these physical and biological mechanisms cannot yet be separated quantitatively.

Across all treatments, one pattern held constant: BTEX migration declined with soil depth, with the 0-to-4-centimeter layer consistently showing the strongest movement and retention. This depth dependence suggests that in real estuarine settings, contaminated surface sediments may act as long-term secondary pollution sources, slowly releasing hydrocarbons toward deeper aquifers at rates dictated by the local salinity, pH, organic carbon inventory, and nutrient status. The single-factor design—holding all other conditions constant while varying one variable at a time, with three replicate columns per treatment and results reported as means plus or minus standard deviations—allows each factor’s independent effect to be isolated, although the authors acknowledge that real estuaries involve interacting gradients that will require multi-factor and long-term simulation studies to fully capture.

The practical stakes are considerable. Groundwater contamination in coastal zones threatens drinking supplies, aquaculture, and ecosystems, and BTEX compounds are toxic, mobile, and volatile, with several components classified as serious health hazards. By demonstrating that higher salinity and nitrate loading actually retard BTEX migration while organic-rich sediments act as sinks, the study suggests that risk models built on inland assumptions may overestimate or underestimate threats in estuarine contexts depending on local chemistry. Conversely, acidification—whether from pollution or environmental change—could mobilize contaminants that were previously locked in organic matter. As coastal aquifers worldwide face intensifying development pressure and seawater intrusion, work like this provides the mechanistic foundation for smarter site screening, targeted remediation, and early-warning systems for organic groundwater pollution in the delicate land–sea interface.