首页> 外文期刊>Soil Biology & Biochemistry >Soil particle surface electrochemical property effects on abundance of ammonia-oxidizing bacteria and ammonia-oxidizing archaea, NH4+ activity, and net nitrification in an acid soil
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Soil particle surface electrochemical property effects on abundance of ammonia-oxidizing bacteria and ammonia-oxidizing archaea, NH4+ activity, and net nitrification in an acid soil

机译:土壤颗粒表面电化学性质对酸性土壤中氨氧化细菌和氨氧化古菌的丰度,NH4 +活性以及净硝化的影响

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Soil surface electrochemical properties may have a strong influence on nitrifying microorganisms, H+ and NH4+ activities, and therefore on the nitrification process. A gradient of surface electrochemical parameters was obtained by amendment of a subtropical acid pine soil (Oxisol) with 0% (control), 3%, 5%, 8%, 10% and 12% pure Ca-Montmorillonite by weight. The H+ and NH4+ activities, the abundance of the ammonia-oxidizing bacterial (AOB) and archaeal (AOA) amoA gene copies, and time-dependent kinetics of net nitrification were investigated. Soil particle surface specific area ranged from 53 to 103 m(2) g(-1) and increased with increasing montmorillonite application rate. Similar to specific area, surface charge quantity, surface charge density, electric field strength and surface potential increased after montmorillonite amendment. The H+ and NH4+ activities decreased linearly after montmorillonite addition. AOB amoA gene copy number was 1.82 x 10(5) copies g(-1) for unamended soil, and the highest AOB amoA gene copy numbers were found for the 10% montmorillonite amendment (3.11 x 10(7) g(-1) soil), which was more than 150 times higher than unamended soil. AOA amoA gene copy numbers were 9.19 x 10(3) copies g(-1) dry unamended soil, and the highest AOA amoA gene copy numbers were found in the 8% montmorillonite amendment (1.22 x 10(5) g(-1) soil). Although pH significantly decreased during the first three weeks of incubation, no significant difference was observed between the unamended control and different rates of montmorillonite addition treatments during the whole incubation. The largest net nitrification (103 mg N kg(-1)) was observed in the 10% montmorillonite amendment and the lowest in unamended soil (62 mg N kg(-1)). While montmorillonite did not change the kinetic patterns of net nitrification, the highest nitrification potential (275 mg N kg(-1)) for the 10% montmorillonite treatment was more than 3 times higher than unamended soil from simulation of time-dependent kinetics. Nitrification was significantly stimulated after montmorillonite amendment in acid soil mainly due to an increase in the quantity and activity of AOB and AOA. We concluded that soil particle surface parameters can significantly influence nitrification, especially in acid soils
机译:土壤表面的电化学性质可能对硝化微生物,H +和NH4 +活性有很大影响,因此对硝化过程也有很大的影响。通过用0%(对照),3%,5%,8%,10%和12%(重量)的纯钙蒙脱土对亚热带酸松土壤(Oxisol)进行改性,可获得表面电化学参数的梯度。研究了H +和NH4 +的活性,氨氧化细菌(AOB)和古细菌(AOA)amoA基因拷贝的丰度以及净硝化的时间依赖性动力学。土壤颗粒表面比表面积范围从53到103 m(2)g(-1),并且随着蒙脱土施用率的增加而增加。蒙脱石改性后,表面电荷量,表面电荷密度,电场强度和表面电势与比表面积相似。添加蒙脱石后,H +和NH4 +活性呈线性下降。未经修饰的土壤的AOB amoA基因拷贝数为1.82 x 10(5)拷贝g(-1),发现10%蒙脱土修饰物的AOB amoA基因拷贝数最高(3.11 x 10(7)g(-1)土壤),比未修正的土壤高150倍以上。 AOA amoA基因拷贝数为9.19 x 10(3)拷贝g(-1)干燥的未改良土壤,并且在8%蒙脱土改良剂(1.22 x 10(5)g(-1)中发现最高的AOA amoA基因拷贝数泥)。尽管在培养的前三周内pH值显着降低,但在整个培养过程中,未修饰的对照和蒙脱石添加处理的不同速率之间未观察到显着差异。在10%蒙脱土改良剂中观察到最大的净硝化(103 mg N kg(-1)),在未改良的土壤中观察到最低的净硝化(62 mg N kg(-1))。虽然蒙脱石不会改变净硝化的动力学模式,但从时变动力学模拟来看,10%蒙脱石处理的最高硝化潜能(275 mg N kg(-1))比未改良土壤高3倍以上。在酸性土壤中蒙脱石改性后,硝化作用得到了显着刺激,这主要是由于AOB和AOA的数量和活性增加所致。我们得出的结论是,土壤颗粒表面参数可以显着影响硝化作用,尤其是在酸性土壤中

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