### Passage
A team of geobiologists investigated the role of the soil bacterium *Bacillus subtilis* and soil humic acids on the dissolution rate of calcite (), a common carbonate mineral. Five experimental trials were conducted at for 14 days. In each trial, 10.0 grams of calcite was placed in a reaction vessel containing 500 mL of an aqueous solution. The dissolution rate was determined by measuring the cumulative concentration of calcium ions () released into the solution. The experimental setups are detailed below:
* Trial 1: Sterile deionized water (pH ), no bacteria.
* Trial 2: Aqueous solution containing of humic acids (pH ), no bacteria.
* Trial 3: Sterile deionized water (pH ) inoculated with of living *B. subtilis*.
* Trial 4: Aqueous solution containing of humic acids (pH ) inoculated with of living *B. subtilis*.
* Trial 5: Aqueous solution containing of humic acids (pH ) inoculated with of heat-killed *B. subtilis*.
To determine if the enhancement of calcite dissolution in the presence of humic acids is specifically driven by the active metabolic processes of living *B. subtilis* rather than the passive physical presence of bacterial cell structures, researchers must compare Trial 4 to a control group. Which trial serves as the most appropriate control group for this comparison, and why?
- ATrial 2, because it contains humic acids but lacks the bacterial cells entirely, isolating the chemical effect of the acid.
- BTrial 3, because it contains living bacteria in deionized water, isolating the effect of bacterial viability in a neutral environment.
- Trial 5, because it contains heat-killed bacteria in humic acids, isolating the effect of active metabolic processes from the physical presence of bacterial cell structures.Answer
- DTrial 1, because it contains only sterile water, providing a baseline for calcite dissolution under completely abiotic and neutral conditions.