Ministry of Agriculture Key Laboratory of Plant Nutrition and Fertilizer, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, PR China.
Institute of Plant Nutrition and Environmental Resources Science, Henan Academy of Agricultural Sciences, Zhengzhou, PR China.
PLoS One. 2018 Sep 12;13(9):e0202660. doi: 10.1371/journal.pone.0202660. eCollection 2018.
In order to study the linkages between straw decomposition rate and the change in soil biological properties after straw addition to different fertilized soils, we collected soils from three long-term fertilization treatments (no-fertilizer, CK; nitrogen, phosphorus, and potassium fertilizers, NPK; NPK plus straw (S), NPKS), and incubated maize straw with these soils at 25°C for 75 days. The average straw carbon dioxide (CO2) emission rate in the CK+straw (S), NPK+S, and NPKS+S treatments was 0.58±0.51, 0.66±0.53, and 0.74±0.58 μg C g-1soil h-1, respectively. The average increase in the contents of fungi, bacteria, and Actinomycetes under straw addition treatments than the control soils (CK, NPK, and NPKS, respectively) changed in the order of CK+S≤NPK+S <NPKS+S, while bacteria and Actinomycetes peaked later in the CK+SthanNPK+S and NPKS+S treatments. Bacterial abundance unchanged, Actinomycetes abundance decreased, but fungal abundance significantly increased in soils after straw addition. The average increase in the activities of β-glucosidase (BG), β-D-cellobiosidase (CB), and β-xylosidase (XYL) differed as: CK+S<NPK+S ≤ NPKS+S, and the highest activities and increments of them occurred later in the CK+S than NPK+S and NPKS+S treatments. Straw CO2 emission rate was poorly correlated with changes in the contents of microbial fractions across all straw addition treatments, but it was significant positively correlated with the increased activities of BG, CB, and XYL under the NPK+S and NPKS+S treatments. Our results indicated that chemical fertilization and straw return soils differently increased straw decomposition because of the different increases in microbial fractions and soil enzyme activities when compared to the no-fertilizer soil, and the decomposition process was more closely correlated with C-obtaining enzymes than microbial fractions.
为了研究秸秆分解率与秸秆添加到不同施肥土壤后土壤生物学特性变化之间的联系,我们采集了来自三种长期施肥处理(不施肥,CK;氮、磷、钾肥料,NPK;NPK 加秸秆(S),NPKS)的土壤,并在 25°C 下用这些土壤培养玉米秸秆 75 天。CK+S、NPK+S 和 NPKS+S 处理中秸秆二氧化碳(CO2)排放率的平均值分别为 0.58±0.51、0.66±0.53 和 0.74±0.58 μg C g-1soil h-1。与对照土壤(CK、NPK 和 NPKS)相比,秸秆添加处理下真菌、细菌和放线菌含量的平均增加顺序为 CK+S≤NPK+S<NPKS+S,而细菌和放线菌的峰值出现在 CK+S 比 NPK+S 和 NPKS+S 处理中。细菌丰度不变,放线菌丰度降低,但秸秆添加后土壤中真菌丰度显著增加。β-葡萄糖苷酶(BG)、β-D-纤维二糖酶(CB)和β-木糖苷酶(XYL)活性的平均增加量分别为:CK+S<NPK+S ≤ NPKS+S,且在 CK+S 中最高,在 NPK+S 和 NPKS+S 处理中出现的时间较晚。秸秆 CO2 排放率与所有秸秆添加处理中微生物区系含量的变化相关性较差,但与 NPK+S 和 NPKS+S 处理中 BG、CB 和 XYL 活性的增加呈显著正相关。我们的结果表明,与不施肥土壤相比,化学施肥和秸秆还田通过不同的微生物区系和土壤酶活性的增加来增加秸秆分解,而分解过程与 C 获得酶的相关性比微生物区系更密切。