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Preprints
https://doi.org/10.5194/egusphere-2024-2796
https://doi.org/10.5194/egusphere-2024-2796
23 Sep 2024
 | 23 Sep 2024

Depth Effects of Long-term Organic Residue Application on Soil Organic Carbon Stocks in Central Kenya

Claude Raoul Müller, Johan Six, Daniel Mugendi Njiru, Bernard Vanlauwe, and Marijn Van de Broek

Abstract. In arable soils, a substantial portion of soil organic carbon (SOC) is stored below the plough layer. To develop sustainable soil management strategies, it is important to assess how they affect the quantity of SOC stored in the subsoil. Therefore, we investigated the impact of organic and inorganic nutrient inputs on SOC stocks down to 70 cm depth in a long-term field trial in Embu, Kenya. There were 3 organic input treatments (manure, Tithonia diversifolia residues, and maize stover) and a control treatment, each with and without the application of mineral nitrogen. These different treatments were applied to a maize monoculture over 38 growing seasons (19 years). Our results show that manure application had the largest positive impact on SOC stocks compared to the control, which was observed down to 60 cm depth. In contrast, Tithonia diversifoliaand maize stover significantly increased SOC compared to the control only within the top 20 cm and 40 cm, respectively. Among the three organic residue treatments, only the application of manure had a significant effect on the SOC stock of the subsoil (i.e., the 30–70 cm depth layer). However, when considering the whole measured profile (i.e., 0–70 cm), all treatments led to significantly higher SOC stocks compared to the 91 ± 12 t C ha-1 of the control: manure had the highest stocks (120 ± 24 t C ha-1), followed by maize stover (112 ± 17 t C ha-1) and tithonia diversifolia (105 ± 11 C t ha-1). Mineral nitrogen application did not have a significant impact on SOC stocks down to 70 cm depth. Overall, our findings indicate that the subsoil in the studied agroecosystems is affected by the type of added organic amendments. Our results imply that gathering knowledge on the soil below the typically studied 0–30 cm depth layer will improve the overall assessment of agroecosystem properties, which is necessary to optimize soil system resilience, limit organic matter losses and improve crop productivity.

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We studied how different organic and inorganic nutrient inputs affect soil organic carbon (SOC)...
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