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Effect of Natural Aging of Biochar on Soil Enzymatic Activity and Physicochemical Properties in Long-Term Field Experiment
Agronomy ( IF 3.3 ) Pub Date : 2020-03-24 , DOI: 10.3390/agronomy10030449
Barbara Futa , Patryk Oleszczuk , Sylwia Andruszczak , Ewa Kwiecińska-Poppe , Piotr Kraska

The effect of different rates of biochar on selected soil properties and enzymatic activity 48, 60, and 72 months after biochar application to soil was investigated. Soil enzymatic activity (dehydrogenase—ADh; phosphatase—Aph; urease—AU), the organic carbon content (TOC), the total nitrogen content (Nt), the mineral nitrogen content (NH4+, NO3), and soil pH were determined. The study was conducted on Haplic Podzol originating from glaciofluvial fine-grained loamy sand. Biochar was applied to soil under winter rye (Secale cereale L.) at rates of 10 (BC10), 20 (BC20), and 30 t ha−1 (BC30). Plots with biochar-unamended soil were the control treatment (BC0). The pH, TOC, and Nt content in the biochar-amended soil were higher compared to the control soil. A broader C:N ratio was found in the BC0 soil compared to BC10, BC20, and BC30. With increasing biochar rate, the content of the ammonium nitrogen form (NH4+) decreased and was statistically lower than in the control soil (BC0). The soil in the BC20 and BC30 treatments was characterized by the highest content of NO3-, whereas the lowest nitrate nitrogen content was found in the control soil (BC0). Biochar application increased soil enzymatic activity. Dehydrogenase activity increased with increasing biochar rate. As far as phosphatase and urease activity is concerned, a similar relationship was not observed. In this case, the soil amended with biochar at a rate of 20 t ha−1 (BC20) was characterized by the highest phosphatase and urease activity.

中文翻译:

生物炭自然老化对长期田间试验土壤酶活性和理化特性的影响

研究了不同生物炭比率对生物炭施用到土壤后48、60和72个月对选定土壤特性和酶活性的影响。土壤酶活性(脱氢酶-ADH;磷酸酶APH;脲酶AU)中,有机碳含量(TOC),总氮含量(N),矿物氮含量(NH 4 +,NO 3 - ),和土壤测定pH。这项研究是对源自河道细粒壤质砂的Haplic Podzol进行的。将生物炭以10(BC 10),20(BC 20)和30 t ha -1(BC 30)的比例施用于冬天黑麦(Secale graine L.)下的土壤)。含生物炭改良土壤的样地为对照处理(BC 0)。pH值,TOC,和N相比于对照土壤中生物炭修订的土壤中的含量较高。与BC 10,BC 20和BC 30相比,在BC 0土壤中发现了更宽的C:N比。随着生物炭速率的增加,铵态氮形式(NH 4 +)的含量降低,且统计学上低于对照土壤(BC 0)。BC 20和BC 30处理的土壤特征在于NO 3-的含量最高,而对照土壤中的硝酸盐氮含量最低(BC 0)。生物炭的施用增加了土壤的酶活性。脱氢酶活性随着生物炭速率的增加而增加。就磷酸酶和脲酶活性而言,未观察到类似的关系。在这种情况下,以20 t ha -1(BC 20)的速率对生物炭进行改良的土壤具有最高的磷酸酶和脲酶活性。
更新日期:2020-03-24
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