Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China.
Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China.
Sci Total Environ. 2016 Jan 15;541:230-237. doi: 10.1016/j.scitotenv.2015.09.080. Epub 2015 Sep 25.
Afforestation may alter soil microbial community structure and function, and further affect soil carbon (C) and nitrogen (N) dynamics. Here we investigated soil microbial carbon and nitrogen (MBC and MBN) and microbial community [e.g. bacteria (B), fungi (F)] derived from phospholipid fatty acids (PLFAs) analysis in afforested (implementing woodland and shrubland plantations) and adjacent croplands in central China. Relationships of microbial properties with biotic factors [litter, fine root, soil organic carbon (SOC), total nitrogen (TN) and inorganic N], abiotic factors (soil temperature, moisture and pH), and major biological processes [basal microbial respiration, microbial metabolic quotient (qCO2), net N mineralization and nitrification] were developed. Afforested soils had higher mean MBC, MBN and MBN:TN ratios than the croplands due to an increase in litter input, but had lower MBC:SOC ratio resulting from low-quality (higher C:N ratio) litter. Afforested soils also had higher F:B ratio, which was probably attributed to higher C:N ratios in litter and soil, and shifts of soil inorganic N forms, water, pH and disturbance. Alterations in soil microbial biomass and community structure following afforestation were associated with declines in basal microbial respiration, qCO2, net N mineralization and nitrification, which likely maintained higher soil carbon and nitrogen storage and stability.
造林可能会改变土壤微生物群落结构和功能,并进一步影响土壤碳(C)和氮(N)动态。在这里,我们调查了来自磷脂脂肪酸(PLFA)分析的造林(实施林地和灌丛种植园)和中国中部邻近农田的土壤微生物碳和氮(MBC 和 MBN)以及微生物群落[例如细菌(B),真菌(F)]。微生物特性与生物因素[凋落物,细根,土壤有机碳(SOC),总氮(TN)和无机 N],非生物因素(土壤温度,水分和 pH)以及主要生物过程[基础微生物呼吸,微生物代谢商(qCO2),净氮矿化和硝化]之间的关系。由于凋落物输入增加,造林土壤的平均 MBC,MBN 和 MBN:TN 比农田更高,但由于低质量(更高的 C:N 比)凋落物,MBC:SOC 比更低。造林土壤的 F:B 比也更高,这可能归因于凋落物和土壤中较高的 C:N 比,以及土壤无机 N 形式,水分,pH 和干扰的变化。造林后土壤微生物生物量和群落结构的变化与基础微生物呼吸,qCO2,净氮矿化和硝化作用的下降有关,这可能维持了较高的土壤碳和氮储存和稳定性。