首页|黄土区农田土壤细菌和真菌群落对长期施氮的响应特征

黄土区农田土壤细菌和真菌群落对长期施氮的响应特征

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[目的]细菌和真菌是调控土壤生态功能的重要因素,摸清细菌和真菌群落的变化有助于深入理解微生物在生态功能中的调节作用.[方法]黄土区渭北旱塬定位监测试验始于1984年.2022年选择其中5个不同施氮(N)量处理小区:0、45、90、135 和 180 kg/hm2(分别记作N0、N45、N90、N135 和N180),采集 0-20 cm土层样品,采用 16S rRNA和ITS高通量测序方法,分析细菌和真菌群落结构及其功能变化,同时测定土壤碳组分、微生物活性、根系生物量及土壤酶活性等.[结果]随着施氮量增加,土壤微生物量从 113 mg/kg增加到 177~234 mg/kg,微生物活性从 4.92 g/(m2·s)增加到 5.83~7.26 g/(m2·s),土壤植物根系量从 1.73 t/hm2 增加到 2.32~2.98 t/hm2.施氮处理土壤细菌群落丰富度(Chao1)和多样性(Shannon)显著降低,分别下降 4.0%~12.3%和 1.6%~1.8%,但真菌群落丰富度和多样性无显著变化.施氮处理土壤变形菌门、芽单胞菌门、拟杆菌门相对丰度分别下降了 2.4%~16.4%、2.1%~26.3%、24.1%~50.0%,细菌中座囊菌纲、伞菌纲相对丰度分别下降了 29.4%~58.8%、44.4%~88.9%,而放线菌门、酸杆菌门、绿湾菌门等细菌相对丰度提高了 10.4%~34.7%、37.8%~54.1%、14.3%~28.6%,子囊菌门、银耳纲等真菌的相对丰度分别提高了8.3%~73.8%、18.2%~45.5%.施氮后,土壤有机碳含量由 6.50 g/kg提升到 7.00~7.35 g/kg,可溶性有机碳含量由 22.43 mg/kg提高到 27.60~34.87 mg/kg,NO3--N含量由 1.38 mg/kg提高到 1.78~2.25 mg/kg,C/N由 8.90 下降到8.64~7.74,微生物的硝化作用显著提高了 14.3%~39.6%,好氧氨氧化功能提高了 25.1%~48.2%,参与碳循环功能的木糖苷酶活性提高了 13.5%~39.3%,纤维二糖水解酶活性提高了 50.3%~126.8%.细菌丰富度和多样性变化与土壤有机碳(SOC)、可溶性有机碳、NO3--N含量和C/N有关.施氮条件下细菌变形菌门丰度降低与土壤可溶性有机碳(DOC)含量升高有关,而放线菌丰度升高与SOC、DOC和NO3--N含量的升高有关,但子囊菌和担子菌的丰度变化与土壤理化性质间的关系不显著.[结论]在黄土高原地区,细菌群落结构对氮肥施用的响应较真菌更为敏感.细菌群落组成的变化与土壤有机碳、可溶性有机碳和NO3--N呈显著正相关,与全氮和C/N呈显著负相关.此外,氮肥施用增加了土壤中与碳循环相关的功能菌丰度,促进了木糖苷酶和纤维二糖水解酶的分泌.
Responses of bacterial and fungal community to long-term nitrogen application in Loess Plateau
[Objectives]The community variation of bacteria and fungi are crucial factors deciding soil ecological functions.We studied the response of bacterial and fungal communities and their functional roles to long-term nitrogen application levels in Loess Plateau,China.[Methods]The soil samples were collected in 2022 from the five N application treatment plots of a long-term experiment,which was in the State Key Agro-Ecological Experimental Station in Changwu County,established in 1984.The N application rates in the five selected treatments were 0,45,90,135,and 180 kg/hm2(denoted as N0,N45,N90,N135,and N180).The bacterial and fungal community structures,soil enzyme activities related to carbon cycling,and soil properties were determined,and the changes relative to the initial of experiment were calculated.[Results]N application led to significant changes in soil chemical properties and microbial population and community structures.Compared to the initials,long term N application increased soil microbial biomass carbon from 113.0 to 177.5-234.0 mg/kg,microbial activity from 4.92 to 5.83-7.26 g/(m2·s),and plant root biomass from 1.73 to 2.32-2.98 t/hm2,decreased bacterial community richness and diversity index(Chao1 and Shannon)by 4.0%-12.3%and 1.6%-1.8%,respectively,did not changed fungal communities obviously.N application significantly decreased the relative abundance of Proteobacteria,Gemmatimonadetes,Bacteroidetes,Dothideomycetes,and Agaricomycetes by 2.4%-16.4%,2.1%-26.3%,24.1%-50.0%,29.4%-58.8%,and 44.4%-88.9%,respectively,but increased the relative abundance of Actinobacteria,Acidobacteria,Chloroflexi,Ascomycota,and Tremellomycetes by 10.4%-34.7%,37.8%-54.1%,14.3%-28.6%,8.3%-73.8%,and 18.2%-45.5%.N application elevated soil organic C(SOC)from initial 6.50 g/kg to 7.00-7.35 g/kg,dissolved organic C(DOC)from 22.43 mg/kg to 27.60-34.87 mg/kg,NO3--N from 1.38 mg/kg to 1.78-2.25 mg/kg,and decreased C/N from 8.90 to 8.64-7.74.With the increase of N application rate,the soil nitrification increased by 14.3%to 39.6%,aerobic ammonia oxidation functions increased by 25.1%-48.2%,and the activities of xylanase increased by 13.5%to 39.3%,and that of cellobiose hydrolase increased by 50.3%to 126.8%.The changes of soil bacterial richness and diversity were correlated with that of SOC,DOC,NO3--N,and C/N ratios.The Proteobacteria abundance was negatively linked to DOC levels,Actinobacteria abundance was positively associated with SOC,DOC,and NO3--N contents,Ascomycota and Basidiomycota abundances were not significantly correlated with soil physiochemical properties.[Conclusions]In Loess Plateau,bacteria structures are more sensitive than fungal structure to N application rate.The changes of bacterial community composition are positively correlated with soil organic matter,dissolved organic carbon and NO3--N,and negatively correlated with total nitrogen and C/N.Nitrogen application increased the abundance of functional bacteria related to carbon cycle in soil and promoted the secretion of xylosidase and cellobiohydrolase.

nitrogen application ratetotal nitrogenC/Nenzymatic activitymicrobial community structure

张薇、王润泽、李彤彤、郭苗苗、郭胜利、王蕊

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西北农林科技大学水土保持研究所,陕西杨凌 712100

中国科学院水利部水土保持研究所,陕西杨凌 712100

施氮量 全氮 碳氮比 酶活性 微生物群落结构

国家重点研发计划国家自然科学基金

2021FY10050242107360

2024

植物营养与肥料学报
中国植物营养与肥料学会

植物营养与肥料学报

CSTPCD北大核心
影响因子:2.331
ISSN:1008-505X
年,卷(期):2024.30(2)
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