Ammonia-oxidizing archaea and bacteria (AOA, AOB) are important contributors to soil ecosystem function, as they convert nitrogen (N) as ammonium (NH4+) into nitrate (NO3-), a more readily available form for plant uptake. This study examines the abundance of AOA and AOB in forest soils of the Pacific Northwest that have experienced wildfire 31, 7, and 5 years previously. Charcoal, a common residue of wildfire, may play a significant role in stimulating nitrification in soils, possibly by adsorbing monoterpenes that may inhibit mono-oxegynase activity in nitrifying organisms. The goal of this study was twofold. We first hypothesized that charcoal would increase the quantity and quality of AOB and/or AOA in wildfire-affected soils. To test this hypothesis, we extracted and compared DNA between burned and unburned sites using real-time quantitative polymerase chain reaction (RT-qPCR). We expect to find a greater abundance of AOA and AOB nucleotides in the burned sites indicated by qPCR, and a larger array of species indicated by DGGE analysis. Secondly, we will introduce monoterpenes (α-pinene) into soils with charcoal present, and soils void of charcoal to assess the interaction between the terpenes and charcoal surfaces. We hypothesize that the addition of terpene will readily adsorb onto charcoal surfaces. Therefore, burned soils will show reduced nitrification inhibition compared to soils without charcoal present and result in higher nitrification rates. These data will be matched with an assessment of the AOA and AOB from the burned and unburned soils, with and without the addition of charcoal in order to reach a better understanding of wildfire effects on forest soils.