To investigate the relationship between the structural characteristics of rough single fracturesand the electrical properties of the rock. In this study, a series of physical models of roughand smooth single fractures were established using the finite element method and Ohm's lawto test the electrical conductivity. By varying the distance between the fracture surfaces, arange of individual fractures with different surface roughness characterized by the relativestandard deviation (RSD) was generated using COMSOL Multiphysics software.Subsequently, the intensity of current passing through the fractures and the influence of roughsurfaces on rock electrical properties were monitored. Numerical simulations demonstrated anon-linear relationship between the current intensity through the models and the RSDroughness, with the equivalent resistivity of the fractured rock increasing with higher RSDvalues. As the RSD roughness increased, the difference in equivalent resistivity betweenrough and smooth fractures also increased, indicating a greater impact of rough surfaces onelectrical properties. The equivalent resistivity of the rock model was 1.05-1.45 times that ofthe parallel plate model with same average aperture. The novelty of this study lies in directlyinvestigating the relationship between roughness of single fractures and rock electricalproperties in three-dimensional, providing insights for understanding the electrical behaviorof rock fractures. / För att undersöka sambandet mellan strukturella egenskaper hos ojämna enkelstrålar och deelektriska egenskaperna hos bergarten. I denna studie etablerades en serie fysiska modeller avojämna och jämna enkelstrålar genom att använda finita elementmetoden och Ohms lag föratt testa elektrisk ledningsförmåga. Genom att variera avståndet mellan strålytornagenererades en rad individuella strålar med olika ytjämnhet som karakteriseras av relativstandardavvikelse (RSD) med hjälp av COMSOL Multiphysics-programvara. Därefterövervakades intensiteten av ström som passerade genom strålarna och inflytandet av ojämnaytor på bergens elektriska egenskaper. Numeriska simuleringar visade på ett icke-linjärtsamband mellan strömintensiteten genom modellerna och RSD-ytjämnheten, där denekvivalenta resistiviteten hos den spruckna bergarten ökade med högre RSD-värden. NärRSD-ytjämnheten ökade, ökade även skillnaden i ekvivalent resistivitet mellan ojämna ochjämna strålar, vilket indikerar en större påverkan av ojämna ytor på de elektriskaegenskaperna. Den ekvivalenta resistiviteten hos bergmodellen var 1,05–1,45 gånger högreän den hos parallellplattanmodellen med samma genomsnittliga apertur. Nyheten i dennastudie ligger i att direkt undersöka sambandet mellan ytjämnheten hos enkelstrålar ochbergens elektriska egenskaper på en tredimensionell skala, vilket ger värdefulla insikter föratt förstå det elektriska beteendet hos bergstrålar och ytterligare förbättra modeller.

<p>To increase the understanding of contaminant transport, specifically biocolloid transport in fractured media, a series of experiments were conducted on single saturated fractures. Hydraulic and solute tracer tests were used to characterize three separate fractures: one natural fracture and two synthetic fractures. Zeta potentials are reported showing the high negative electric charge of the synthetic fractures relative to the natural fractures in the phosphate buffer solution (PBS) used during the biocolloid tracer tests.</p> <p><em>E. coli</em> RS2-GFP tracer tests were conducted on all three fractures at specific discharges of 5 m/d, 10 m/d and 30 m/d. Lower <em>E. coli</em> recovery was consistently observed in the natural fracture, due to 1) attachment because of the lower negative charge of the natural fracture relative to the synthetic fracture; and 2) the presence of dead end fractures within the fracture matrix. In the synthetic fractures, where surface charges were equal, in the larger, more variable fracture aperture, lower recoveries were found when compared to the smaller, less variable fracture aperture, which was not expected. This indicates that aperture variability plays a larger role than fracture aperture size in the retention of biocolloids in fractures.</p> <p>Differential transport was consistently observed in all three fractures, but was more prominent in the synthetic fractures. This indicates that charge exclusion plays a more dominant role in the differential transport of colloids than size exclusion, though size exclusion cannot be eliminated as a retention mechanism based on these experiments. Differential transport was also heavily influenced by specific discharge as the difference in arrival times between the bromide and <em>E. coli</em> increased in all three fractures as the specific discharge decreased.</p> <p>Visualization tests were completed on the synthetic fractures showing the location of multiple preferential flow paths, as well as areas with low flow.</p>