铁肥与稻田土壤固碳

IF 3.9 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Biogeochemistry Pub Date : 2024-10-08 DOI:10.1007/s10533-024-01183-7
Snowie Jane C. Galgo, Lorraine Joule B. Estrada, So Yeong Park, Ronley C. Canatoy, Muhammad Israr Khan, Benjamin L. Turner, Pil Joo Kim
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引用次数: 0

摘要

海洋中的铁(Fe)肥通过在浮游植物中封存二氧化碳(CO2)来减缓全球变暖,但铁肥对耕地土壤中碳(C)封存的影响仍然未知。铁通常作为高炉渣(BFS)被添加到稻田中,高炉渣是钢铁制造的副产品,用作硅(Si)肥料以提高生产力。然而,高炉矿渣中还含有大量的铁氧化物,可能会通过与有机物形成复合物而促进碳固存。为了研究这个问题,我们首先分析了韩国全国土壤调查的数据,以估算通过 BFS 持续添加铁对土壤有机碳(SOC)储量的影响。结果显示,SOC 与可提取的铁和可利用的硅浓度之间存在很强的正相关性,这表明定期施用硅酸盐肥料有助于增加 SOC 储量。其次,为了分离铁添加量对 SOC 储量的影响,我们用富含氧化铁(0-5%,重量比-1)的 BFS 进行了培养试验。施用硅酸盐肥料后,土壤呼吸作用明显降低,而富含铁的肥料则加强了这种作用。最后,为了验证添加铁元素对田间 SOC 储量变化的影响,我们在稻田中添加了三种不同的富含铁元素的硅酸盐肥料,并通过生态系统净 C 预算(NECB)估算量化了 SOC 储量变化。施用硅酸盐肥料后,净初级生产力(NPP)比对照组明显提高了 18-20%,而且这种效应随着铁元素添加量的增加而增强。施用硅酸盐肥料后,土壤呼吸作用比对照组降低了 15-30%,铁元素的富集进一步加强了这种效应。因此,在水稻种植期间施用硅酸盐肥料可使 SOC 储量比对照增加 0.65-0.68 兆克碳/公顷,而施用富铁肥料可使 SOC 储量增加 0.90-0.96 兆克碳/公顷。总之,添加 BFS 对 SOC 储量的积极影响部分与氧化铁的作用有关,主要是通过抑制土壤呼吸作用。因此,富含铁的硅酸盐肥料为增加稻田中的 SOC 储量和作物产量提供了一种管理策略。
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Iron fertilization and soil carbon sequestration in rice paddies

Iron (Fe) fertilization of the ocean mitigates global warming by sequestering carbon dioxide (CO2) in phytoplankton, but the effect of Fe fertilization on carbon (C) sequestration in arable soils remains unknown. Iron is often added to rice paddies as blast furnace slag (BFS), a byproduct of steel manufacturing used as a silicon (Si) fertilizer to improve productivity. However, BFS also contains large amounts of Fe oxides, which might promote C sequestration by forming complexes with organic matter. To investigate this, we first analyzed data from a national survey of soils from South Korea to estimate the effect of continuous Fe addition via BFS on soil organic C (SOC) stocks. This revealed a strong positive correlation between SOC and extractable Fe and available Si concentrations, indicating that periodic silicate fertilizer application contributed to an increase in SOC stock. Second, to isolate the effect of Fe addition on SOC stocks, we conducted an incubation test with BFS enriched with Fe oxides (0–5%, wt wt−1). Soil respiration was significantly reduced by silicate fertilizer application, and this effect was strengthened with the Fe-enriched fertilizer. Finally, to verify the effect of Fe addition on SOC stock changes in the field, we added three different Fe-enriched silicate fertilizers to rice paddies and quantified SOC stock changes by net ecosystem C budget (NECB) estimation. Silicate fertilizer significantly increased net primary production (NPP) by 18–20% over the control, and this effect was strengthened with increasing Fe addition. Silicate fertilizer application decreased soil respiration by 15–30% over the control, and this effect was strengthened further by Fe enrichment. As a result, silicate fertilizer application during rice cultivation increased the SOC stock by 0.65–0.68 Mg C ha−1 over the control and by 0.90–0.96 Mg C ha−1 for Fe-enriched fertilizer. In conclusion, the positive effect of BFS addition on SOC stock is related in part to the role of Fe oxides, primarily through the suppression of soil respiration. Fe-enriched silicate fertilizer therefore provides a management strategy to increase SOC stocks and crop productivity in rice paddies.

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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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