其他摘要 | 【Objectives】The fertility change in nutrient contents and microbial structure of farmland after long-
term fertilization was studied in this paper, which would provide theoretical base for reasonable fertilization
practice to maintain a stable and healthy soil ecosystem.【Methods】The investigated farmland was from a 28-
years’ long-term fertilization experiment in the “National Monitoring Base of Soil Fertility and Fertilizer
Efficiency on Loess Soil” in Yangling Demonstration Zone, Shaanxi Province, where the cropping system was
winter wheat-summer fallow and without irrigation. The soil samples were collected from three of the experiment
treatments, namely, no fertilization control (CK), pure chemical fertilizer (NPK, N–P 2 O 5 –K 2 O=135–108–67.5 kg/hm 2 )
and chemical fertilizer and manure combination (MNPK, 70% of N from cattle manure). After harvest of wheat,
soil samples of 0–20 cm in depth were collected. The soil nutrient contents, water content, microbial biomass C
and N contents were determined. The DNA of genome in soil samples were extracted and detected by 1%
agarose gel electrophoresis, and sequenced afterwards. The Shannon, ACE and Chao1 indices were
calculated.【Results】Compared with CK, the NPK and MNPK significantly increased soil organic carbon, total
nitrogen, microbial biomass carbon, microbial biomass nitrogen, nitrate nitrogen and ammonium nitrogen, while
significantly reduced soil pH. The copy number of bacterial genes were 6.69 × 10 9 – 16.46 × 10 9 per gram of dry
soil for the three treatments, and those in NPK and MNPK treatments were 77% and 146% significantly higher
than that in CK. The Shannon diversity index of soil bacteria of MNPK was significantly higher, while Simpson
index were significantly lower than those of CK and NPK treatments, and there was no significant difference
between NPK and CK. The bacterial richness index (Chao1 index and ACE index) and the uniformity index
were not significantly different among the 3 treatments. A total of 35 groups of bacteria were obtained at the
level of phylum, in which Actinobacteria, Proteobacteria, Acidobacteria and Chloroflexi were the main
dominant ones (relative abundance > 10%), and accounted for 80.1%–81.7% of the total bacteria phyla.
Compared with CK, MNPK significantly reduced the relative abundance of Actinomycetes (F = 5.845, P <
0.05) and increased that of Bacteroides (F = 4.461, P < 0.05). There was no significant difference for other phyla
of bacteria among the 3 treatments. The results of redundancy analysis showed that the soil bacterial community
structures were significantly different between no fertilization (CK) and fertilization (NPK and MNPK), and
MNPK had a greater impact than NPK on soil bacterial community composition. The importance of soil physical
and chemical properties affecting the bacterial communities was as follows: nitrate nitrogen > soluble organic
carbon > pH > ammonium nitrogen > organic carbon > soil water content.【Conclusions】In the rain-fed
farmland in Eum-orthic anthrosol area of Guanzhong, the bacteria population, diversity and richness are
significantly improved in soils under long-term balanced chemical fertilization and combination of organic and
inorganic fertilization. Combination of organic and inorganic fertilizers could increase the bacteria diversity that is
more efficient in increasing the abundance of Bacteroides and decreasing that of Actinomycetes, which represents
more stable and healthy in soil ecosystem. |
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