State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Hangzhou 311300, China.
State Key Laboratory of Subtropical Silviculture, Zhejiang A&F University, Hangzhou 311300, China; Tea Research Institute, Chinese Academy of Agricultural Sciences, Hangzhou 311300, China.
Sci Total Environ. 2024 Aug 20;939:173606. doi: 10.1016/j.scitotenv.2024.173606. Epub 2024 May 30.
Organic soil amendments have been widely adopted to enhance soil organic carbon (SOC) stocks in agroforestry ecosystems. However, the contrasting impacts of pyrogenic and fresh organic matter on native SOC mineralization and the underlying mechanisms mediating those processes remain poorly understood. Here, an 80-day experiment was conducted to compare the effects of maize straw and its derived biochar on native SOC mineralization within a Moso bamboo (Phyllostachys edulis) forest soil. The quantity and quality of SOC, the expression of microbial functional genes concerning soil C cycling, and the activity of associated enzymes were determined. Maize straw enhanced while its biochar decreased the emissions of native SOC-derived CO. The addition of maize straw (cf. control) enhanced the O-alkyl C proportion, activities of β-glucosidase (BG), cellobiohydrolase (CBH) and dehydrogenase (DH), and abundances of GH48 and cbhI genes, while lowered aromatic C proportion, RubisCO enzyme activity, and cbbL abundance; the application of biochar induced the opposite effects. In all treatments, the cumulative native SOC-derived CO efflux increased with enhanced O-alkyl C proportion, activities of BG, CBH, and DH, and abundances of GH48 and cbhI genes, and with decreases in aromatic C, RubisCO enzyme activity and cbbL gene abundance. The enhanced emissions of native SOC-derived CO by the maize straw were associated with a higher O-alkyl C proportion, activities of BG and CBH, and abundance of GH48 and cbhI genes, as well as a lower aromatic C proportion and cbbL gene abundance, while biochar induced the opposite effects. We concluded that maize straw induced positive priming, while its biochar induced negative priming within a subtropical forest soil, due to the contrasting microbial responses resulted from changes in SOC speciation and compositions. Our findings highlight that biochar application is an effective approach for enhancing soil C stocks in subtropical forests.
有机土壤改良剂已被广泛应用于增强农林生态系统中的土壤有机碳(SOC)储量。然而,热解和新鲜有机物质对原生 SOC 矿化的对比影响以及介导这些过程的潜在机制仍知之甚少。在这里,进行了一项为期 80 天的实验,以比较玉米秸秆及其衍生生物炭对毛竹林(Phyllostachys edulis)土壤中原生 SOC 矿化的影响。测定了 SOC 的数量和质量、与土壤 C 循环有关的微生物功能基因的表达以及相关酶的活性。玉米秸秆增加了而其生物炭减少了原生 SOC 衍生 CO 的排放。与对照相比,添加玉米秸秆(cf. 对照)增加了 O-烷基 C 比例、β-葡萄糖苷酶(BG)、纤维二糖水解酶(CBH)和脱氢酶(DH)的活性以及 GH48 和 cbhI 基因的丰度,同时降低了芳香族 C 比例、RubisCO 酶活性和 cbbL 丰度;生物炭的应用则诱导了相反的效果。在所有处理中,随着 O-烷基 C 比例、BG、CBH 和 DH 的活性以及 GH48 和 cbhI 基因的丰度的增加,以及芳香族 C、RubisCO 酶活性和 cbbL 基因丰度的降低,原生 SOC 衍生 CO 的累积排放量增加。玉米秸秆促进了原生 SOC 衍生 CO 的排放,这与 O-烷基 C 比例、BG 和 CBH 的活性以及 GH48 和 cbhI 基因的丰度的增加以及芳香族 C 比例和 cbbL 基因丰度的降低有关,而生物炭则产生了相反的效果。我们得出结论,玉米秸秆诱导了正激发效应,而其生物炭则在亚热带森林土壤中诱导了负激发效应,这是由于 SOC 形态和组成的变化导致微生物反应的差异所致。我们的研究结果强调,生物炭的应用是增强亚热带森林土壤碳储量的有效方法。