Buthelezi Kwenama, Buthelezi-Dube Nkosinomusa
School of Agricultural, Earth and Environmental Sciences, University of KwaZulu-Natal, P. Bag X01, Scottsville, Pietermaritzburg 3201, South Africa.
Plants (Basel). 2025 Apr 25;14(9):1302. doi: 10.3390/plants14091302.
This study investigated the long-term (70 years) effects of N fertilisation (ammonium nitrate [AN], ammonium sulphate [AS]) at 70 and 211 kg N kg/ha, and liming (L) on plant-microbial interaction and soil carbon stability in a semi-arid grassland in South Africa. Aboveground biomass increased with N addition, particularly AN211, showing a 119% increase compared to the control, while both liming and N applications increased belowground biomass. Nitrogen addition significantly altered plant stoichiometric ratios, with root N ratios showing greater treatment-induced variation (12.7-51.3) than shoot N ratios (10.2-16.8). Microbial biomass carbon peaked with AN70 treatment, while dehydrogenase activity was highest in lime-only plots but suppressed in non-limed N treatments. Conversely, urease activity was highest in the control group and suppressed in most fertilised treatments. Despite increased biomass production, SOC remained unchanged across treatments (49.7-57.6 g/kg), whereas soil pH was lowest (<3.5) and highest (>6) under N fertilisation and lime, respectively. PCA revealed distinct clustering of treatments, with N forms differentially affecting plant allocation patterns and microbial parameters. This study demonstrates that plant-soil-microbe stoichiometric imbalances and pH-induced limitations on microbial function explain the disconnect between plant productivity and carbon sequestration in this semi-arid grassland ecosystem.
本研究调查了在南非半干旱草原上,施氮量为70和211千克氮/公顷的氮肥(硝酸铵[AN]、硫酸铵[AS])以及施石灰(L)对植物-微生物相互作用和土壤碳稳定性的长期(70年)影响。地上生物量随施氮量增加而增加,尤其是AN211,与对照相比增加了119%,而施石灰和施氮均增加了地下生物量。施氮显著改变了植物的化学计量比,根系氮比显示出比地上部氮比(10.2 - 16.8)更大的处理诱导变化(12.7 - 51.3)。微生物生物量碳在AN70处理时达到峰值,而脱氢酶活性在仅施石灰的地块中最高,但在未施石灰的施氮处理中受到抑制。相反,脲酶活性在对照组中最高,在大多数施肥处理中受到抑制。尽管生物量产量增加,但各处理间土壤有机碳含量保持不变(49.7 - 57.6克/千克),而土壤pH值在施氮和施石灰处理下分别最低(<3.5)和最高(>6)。主成分分析揭示了各处理的明显聚类,氮形态对植物分配模式和微生物参数有不同影响。本研究表明,植物-土壤-微生物化学计量失衡以及pH值对微生物功能的诱导限制解释了该半干旱草原生态系统中植物生产力与碳固存之间的脱节。