Soils are rich in bacteria (1 × 10 2–2 × 109 cells g-1), with live bacterial abundance dependent on a number of physical and chemical properties, such as organic matter, temperature, particle distribution, moisture, and pH. Soil bacteria play a si...
Soils are rich in bacteria (1 × 10 2–2 × 109 cells g-1), with live bacterial abundance dependent on a number of physical and chemical properties, such as organic matter, temperature, particle distribution, moisture, and pH. Soil bacteria play a significant role in global nutrient cycling as well as soil biogeochemistry. There are a number of different methods that have been used to quantify live bacteria in soil. To date, an evaluation of these methods has not been undertaken to identify the most precise and accurate method(s). This study evaluates the conditions of appropriate storage temperature conditions (i.e., -20, 4, 24, 30 °C) and pretreatment methods (i.e., sonication, centrifugation, filtration) for measuring live soil bacterial populations. We also investigated culture-dependent methods (CDMs; i.e., colony forming unit (CFU), spotting, and most probable number (MPN)) and culture-independent/direct counting methods (CIMs; i.e., flow cytometry (FCM), epifluorescence microscopy (EM) count, and DNA extraction). Each method was tested using 72 soil samples collected from a local farm site at three different depths (i.e., 20, 100, and 180 cm). As the storage temperature at 4 °C showed the lowest variation of live bacterial cell number, storage at 4 °C was most appropriate, and the highest number of live bacterial populations was measured with the pretreatment of 3 minutes of sonication time (300 W), 1400 × g of centrifugation speed. Among all CDMs, MPN was found to be rapid, simple, and reliable (low variability amongst triplet). However, the number of bacteria quantified by MPN was 1–2 orders lower than that quantified by CIMs, likely due to the inability of MPN to count anaerobic bacteria. The DNA extraction method appeared to overestimate soil bacterial numbers, which may be attributed to DNA extraction from dead bacteria and free DNA in the soil
- VIII
matrix. FCM was found to be ineffective in counting soil bacteria as it was difficult to separate the bacterial cells from the soil particles. Dyes used in FCM stained the bacterial DNA and clay particles. The EM count was deemed a highly effective method as it provided information on soil mineral particles, live bacteria, and dead bacteria; however, it was a time-consuming and labor-intensive process. Bacterial numbers obtained using CDMs and CIMs were also compared based on soil pH, soil water content, and clay/silt content. Combining both types of methods was considered the best approach to acquire better information on the characteristics of indigenous soil microorganisms (aerobic versus anaerobic, live versus dead), and their spatial link to soil physical and chemical properties.