Variations of soil properties and soil surface loss after fire in rotational shifting cultivation in Northern Thailand
Issued Date
2023-01-01
Resource Type
eISSN
2296665X
Scopus ID
2-s2.0-85171558690
Journal Title
Frontiers in Environmental Science
Volume
11
Rights Holder(s)
SCOPUS
Bibliographic Citation
Frontiers in Environmental Science Vol.11 (2023)
Suggested Citation
Arunrat N., Sereenonchai S., Kongsurakan P., Yuttitham M., Hatano R. Variations of soil properties and soil surface loss after fire in rotational shifting cultivation in Northern Thailand. Frontiers in Environmental Science Vol.11 (2023). doi:10.3389/fenvs.2023.1213181 Retrieved from: https://repository.li.mahidol.ac.th/handle/20.500.14594/90221
Title
Variations of soil properties and soil surface loss after fire in rotational shifting cultivation in Northern Thailand
Other Contributor(s)
Abstract
Since fire is still necessary for rotational shifting cultivation (RSC), the vertical distribution and slope effect on soil properties and soil surface loss after a fire remain unclear. To address these research gaps, the study aims to achieve the following objectives: 1) investigating post-fire soil properties and soil surface loss in RSC, and 2) assessing the vertical distribution and slope effect on soil properties and soil surface loss in RSC. Soil samples were collected from two stages of RSC: 6 years (RSC-6Y) and 12 years (RSC-12Y), located in Chiang Mai Province, Northern Thailand. A continuous 15-year left fallow field (CF-15Y) was used as the reference site. Soil samples were collected from the upper, middle, and lower slopes at depths of 0–5, 5–10, 10–20, and 20–30 cm at five different time points: before burning, 5 min, 3 months, 6 months, and 9 months post-fire. The results indicated that older fallow fields had a tendency to accumulate more soil organic carbon (SOC) and soil organic nitrogen (STN). The color of the ash was altered by the fire, resulting in dark reddish-brown ash with higher levels of pH, organic matter (OM), electrical conductivity, total nitrogen, and soil nutrients when compared to gray and white ashes. The combustion of OM during the fire was found to release soil nutrients, which could explain the increase after burning. SOC stock increased at deeper layers (5–10 cm) with higher values than pre-burning levels, especially at lower slope positions, while STN stock decreased at the surface soil post-fire but increased in deeper layers at all slope positions. The average soil surface loss ranged from 1.6 to 3.1 cm, with the highest loss observed 9 months after the fire (during the rainy season) at the upper slope. In terms of the impact of slope on soil properties following the fire event, our study indicated a significant correlation between lower slopes and variables including SOC, STN, electrical conductivity, nitrate–nitrogen (NO3-N), ammonium nitrogen (NH4-N), exchangeable calcium, and exchangeable magnesium. Further study is required to investigate and develop appropriate post-fire management strategies to effectively reduce nutrient loss and minimize soil surface erosion.