Microbial life-history strategies mediate differential effects of straw and biochar amendments on soil POC/MAOC dynamics and SOC sequestration
Liping Na , Yalin Liu , Qiong Nan , Litian Chen , Da Dong , Weixiang Wu , Jiangwu Tang , Shengmao Yang , Yuxue Liu
Biochar ›› 2026, Vol. 8 ›› Issue (1) : 118
Enhancing soil organic carbon (SOC) sequestration in paddy soils is a critical strategy for climate change mitigation. However, the mechanistic underpinnings of how substrate quality modulates microbial life-history strategies to regulate the formation and stabilization of distinct SOC fractions—particulate organic carbon (POC) and mineral-associated organic carbon (MAOC)—remain poorly understood. We conducted a 65-day incubation experiment using 13C-labeled rice straw and straw-derived biochar to disentangle the relationships among energy inputs, microbial strategies, and SOC stabilization pathways. Both straw and biochar amendments increased SOC content, with biochar inducing a 103% increase compared to only 38.7% from straw. Straw improved nutrient availability (e.g., dissolved organic carbon and microbial biomass carbon) and stimulated the activities of β-glucosidase, β-1,4-N-acetylglucosaminidase, leucine aminopeptidase, and acid phosphatase, thereby enriching r-strategist microbes (e.g., Mortierellomycota and Firmicutes). This promoted fungal-mediated POC formation and MAOC accumulation derived from bacterial necromass. However, straw induced a positive priming effect, accelerating the mineralization of native SOC and resulting in a carbon sequestration efficiency of only 22.8% by day 65. In contrast, biochar alleviated microbial nitrogen demand, redirected microbial activity toward the decomposition of recalcitrant carbon, and enriched K-strategist microbes (Actinobacteriota and Chloroflexi). These shifts further facilitated MAOC accumulation via bacterial necromass formation, while inducing a negative priming effect that minimized native carbon loss, achieving a carbon sequestration efficiency of 99.7% at the end of the incubation. Our findings reveal that straw and biochar enhance SOC sequestration through distinct microbial pathways: straw drives rapid but less efficient carbon accumulation via r-strategist microbial activity, whereas biochar promotes stable and highly efficient sequestration through K-strategist-mediated processes. These results highlight the importance of substrate quality in shaping microbial community dynamics and SOC sequestration outcomes, providing a mechanistic basis for optimizing organic amendment strategies in paddy agroecosystems.
Soil organic matter / Particulate organic matter / Mineral-associated organic matter / r-strategists / K-strategists / Biochar amendment
| [1] |
|
| [2] |
|
| [3] |
|
| [4] |
|
| [5] |
|
| [6] |
|
| [7] |
|
| [8] |
|
| [9] |
|
| [10] |
|
| [11] |
|
| [12] |
|
| [13] |
|
| [14] |
|
| [15] |
|
| [16] |
|
| [17] |
|
| [18] |
|
| [19] |
|
| [20] |
|
| [21] |
|
| [22] |
Helmke PA, Sparks DL (1996) Lithium, sodium, potassium, rubidium, and cesium. Methods of soil analysis, pp 551–574. https://doi.org/10.2136/sssabookser5.3.c19 |
| [23] |
|
| [24] |
|
| [25] |
|
| [26] |
|
| [27] |
|
| [28] |
|
| [29] |
|
| [30] |
|
| [31] |
|
| [32] |
|
| [33] |
|
| [34] |
|
| [35] |
|
| [36] |
|
| [37] |
|
| [38] |
|
| [39] |
|
| [40] |
|
| [41] |
|
| [42] |
|
| [43] |
|
| [44] |
|
| [45] |
Mulvaney RL (1996) Nitrogen—inorganic forms. Methods of soil analysis, pp 1123–1184. https://doi.org/10.2136/sssabookser5.3.c38 |
| [46] |
|
| [47] |
|
| [48] |
|
| [49] |
|
| [50] |
|
| [51] |
|
| [52] |
|
| [53] |
|
| [54] |
|
| [55] |
|
| [56] |
|
| [57] |
|
| [58] |
|
| [59] |
|
| [60] |
|
| [61] |
|
| [62] |
|
| [63] |
|
| [64] |
|
| [65] |
|
| [66] |
|
| [67] |
|
| [68] |
|
| [69] |
|
| [70] |
|
| [71] |
|
| [72] |
|
| [73] |
|
| [74] |
|
| [75] |
|
| [76] |
|
| [77] |
|
| [78] |
|
| [79] |
|
| [80] |
|
| [81] |
|
| [82] |
|
| [83] |
|
| [84] |
|
The Author(s)
/
| 〈 |
|
〉 |