[A-GE30] 地質媒体における流体移動、物質移行 及び環境評価

[AGE30-05] Seasonal variations in soil CO₂ concentrations and fluxes at two different soybean fields

*杉浦 有香¹、濱本 昌一郎¹、二瓶 直登²、平 敏伸³、平山 孝³、松波 寿弥⁴、市橋 泰範⁵、西村 拓¹ (1.東京大学大学院農学生命科学研究科、2.福島大学 食農学類、3.福島県農業総合センター、4.農研機構 東北農業研究センター、5.理化学研究所バイオリソース研究センター)

キーワード：ガス環境、土壌呼吸、モニタリング

Agricultural field is one of the important sources of greenhouse gas emissions. It is known that CO₂ emissions from soils are influenced by environmental factors such as soil moisture, soil temperature, and organic matter content. These factors are variable with different soil types, therefore it is essential to understand the relationship between soil type and soil CO₂ dynamics. Previous studies have also shown that continuous monitoring is required to accurately understand the effects of soil moisture on CO₂ gas emissions. In this study, we aimed to clarify the effect of soil types on CO₂ dynamics in soybean fields. Measurements were conducted in two different soybean fields; volcanic ash soil and lowland soil located in Fukushima City and Koriyama City in Japan, respectively. Each field consisted of three treatments: unplanted (NC), cow manure (CM), and chemical fertilizer (CF). O₂and CO₂ concentrations were monitored at two depths (10 cm, 25 cm) at one-hour intervals during the soybean growing season from June to October in 2021. At both sites, volumetric water content, soil temperature, electrical conductivity, and water potential at four depths (2 cm, 10 cm, 18 cm, and 25 cm) were measured at 30-minute or 1-hour intervals. Basic physical properties, gas diffusion coefficient, air permeability, and water retention curves were measured using undisturbed samples collected at four depths (5 cm, 10 cm, 18 cm, and 25 cm). The measured CO₂ concentrations and gas diffusion coefficients were used to calculate the CO₂ fluxes at depths of 0-10 cm and 10-25 cm. The rate of CO₂ production was evaluated by subtracting CO₂ flux at 10-25 cm depth from the one at 0-10 cm depth.
The difference in time-series variations of CO₂ concentration among soils was small at 10 cm depth, while CO₂ concentration at 25 cm depth was higher in lowland soil than in volcanic ash soil. This was because of the smaller air-filled porosity (i.e., lower gas diffusion coefficient) in the lowland soil than in volcanic ash soil. For the CM plot, the rate of CO₂ production was higher in the volcanic ash soil. Because during the monitoring periods, volcanic ash soil showed higher air-filled porosity than lowland soil, especially at 0-10 cm depth, larger oxygen supply from the atmosphere to soil enhanced soil respiration in the volcanic ash soil. Relations between CO₂ flux at 0-10 cm depth and volumetric water content showed an optimum volumetric water content that maximized CO₂ flux in each field. The optimum water content ranged from 0.5 to 0.6 as water saturation, regardless of the soil type and treatment.