Abstract
Rice husk gasification slag (RS) is a type of biochar that is one of the main by-products generated from the production of biomass power with rice husk as the feed. This study aimed to explore the short-term effect of the application of RS on the movement and transformation of fertilizer P in two different soil types through an incubation experiment. The results showed that the RS addition had a significant influence on the diffusive movement of P in soil microsites close to fertilizer placements both in latosolic red soil and fluvo-aquic soil. After 50 d of incubation, most of the WE-P (water-extractable P), AE-P (acid-extractable P), and Olsen-P (available P) were concentrated within 0–5 mm from the fertilization site. WE-P, Olsen-P, and the movement amount of the P in the 0–5 mm soil section were significantly increased at all levels of the RS application in the fertilizer P both in the two soil types. The application of the RS reduced the sorption and precipitation of the fertilizer P in the soil and improved the efficiency of the fertilizer P. The findings presented in this study may be used as references in developing RS applications that reduce losses of fertilizer P and reduce environmental risks.
Highlights
Due to the sorption, precipitation, and microbial immobilization of soil, most fertilizer P is quickly turned into plant-unavailable forms after application [1,2,3]
The addition of the Rice husk gasification slag (RS) had a significant influence on the diffusive movement of P in soil microsites close to fertilizer placements in the two soil types
The acid-insoluble P accounted for 68.57–69.26% and 57.10–58.40% of the total P application in the latosolic red soil and fluvo-aquic soil, respectively
Summary
Precipitation, and microbial immobilization of soil, most fertilizer P is quickly turned into plant-unavailable forms after application [1,2,3]. The bound P is abundant, but the plant-available form is limited. It is estimated that approximately 40% of the crop productivity of agricultural soils worldwide is limited by P availability, and P deficiency is a common problem [4]. Additional P inputs (mineral P fertilizer, atmospheric deposition, and weathering) and phosphate loss (surface runoff, subsurface flow, leaching, etc.) may result in freshwater and marine resource eutrophication [6,7,8]
Published Version (
Free)
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have