Norgbey Eyram, Murava Raphinos Tackmore, Rajasekar Adharsh, Huang Qiong, Zhou Jin, Robinson Steve
Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control (AEMPC), Collaborative Innovation Center of Atmospheric Environment and Equipment Technology (CIC-AEET), Nanjing University of Information, Science &Technology, Nanjing, 210044, China.
NUIST Reading Academy, Nanjing University of Information, Science &Technology, Nanjing, 210044, China.
Environ Monit Assess. 2022 Jul 11;194(8):575. doi: 10.1007/s10661-022-10229-y.
Anthropogenic deposition of nitrogen (N) and elevated CO (CO) are expected to increase continuously and rapidly in the near future and influence global carbon cycling. These parameters affect the ecosystem by regulating the microbial community and contribute to soil organic matter decomposition. The study was performed to understand the effects of N additions (4 and 6mgl) and CO (700 ppm) on carbon (C)/nitrogen (N) content in the soil, microbial community, and plant biomass (Alternanthera philoxeroides species). The results showed that when the atmospheric CO concentration was raised, the total organic carbon (TOC) in the soil statistically increased (P < 0.05) by 4% and 3% under low and high N additions respectively, while the inorganic carbon content also increased by 1% and 3% (P > 0.05) under the same conditions. The increase in the soil TOC content was a result of the movement of carbon from water to the soil due to the presence of vascular tissues of plants in the water. The redundancy analysis (RDA) results revealed that the presence of plant species was responsible for the carbon content increment in the soil. The plant biomass content increased by 30.96% (P = 0.081) and 31.36%, (P = 0.002) under low and high N addition respectively due to the increment in atmospheric CO. The nitrogen content in the plant species decreased (p > 0.05) by 8.62% and 6.25% at low and high N addition respectively when atmospheric CO was raised. This suggests that soil microbes competed with the plants for inorganic nitrogen in the soil and the microbes used up the inorganic nitrogen before it got to the plants. The gram-positive bacteria and fungi population decreased under high N addition and CO while gram-negative bacteria increased, suggesting that N additions and CO affected the microbial function and correlated with the nitrogen reduction in the soil. The results from this study serve as a guide to researchers and stakeholders in making policies with regard to the constant increasing CO concentration in the atmosphere.
预计在不久的将来,人为的氮(N)沉降和升高的二氧化碳(CO₂)将持续且迅速增加,并影响全球碳循环。这些参数通过调节微生物群落来影响生态系统,并促进土壤有机质分解。本研究旨在了解添加氮(4和6mg/L)和二氧化碳(700ppm)对土壤中碳(C)/氮(N)含量、微生物群落和植物生物量(空心莲子草物种)的影响。结果表明,当大气中二氧化碳浓度升高时,在低氮和高氮添加条件下,土壤中的总有机碳(TOC)分别在统计学上显著增加(P < 0.05)4%和3%,而无机碳含量在相同条件下也分别增加了1%和3%(P > 0.05)。土壤TOC含量的增加是由于水中植物维管组织的存在,使得碳从水转移到土壤的结果。冗余分析(RDA)结果表明,植物物种的存在是土壤碳含量增加的原因。由于大气中二氧化碳的增加,在低氮和高氮添加条件下,植物生物量含量分别增加了30.96%(P = 0.081)和31.36%(P = 0.002)。当大气中二氧化碳升高时,低氮和高氮添加条件下植物物种中的氮含量分别下降(p > 0.05)8.62%和6.25%。这表明土壤微生物与植物竞争土壤中的无机氮,并且微生物在无机氮到达植物之前就将其消耗殆尽。在高氮添加和二氧化碳条件下,革兰氏阳性菌和真菌种群减少,而革兰氏阴性菌增加,这表明添加氮和二氧化碳影响了微生物功能,并与土壤中的氮减少相关。本研究结果为研究人员和利益相关者制定有关大气中二氧化碳浓度持续增加的政策提供了指导。