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Biochar amendment effects on the activities of soil carbon, nitrogen, and phosphorus hydrolytic enzymes: a meta-analysis

机译:生物炭修正对土壤碳,氮和磷水解酶活性的影响:Meta分析

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The aim of this meta-analysis was to synthesize the effects of biochar amendment on soil enzyme activities (SEAs) related to carbon (C), nitrogen (N), and phosphorus (P) cycling. Based on 401 paired comparisons from 43 published studies, the SEAs and main influential factors were analyzed in response to biochar characteristics, soil properties, and experiment conditions. Results showed that biochar additions to soils overall increased the N- and P-cycling SEAs by 14 and 11%, respectively. The enhancement of the N- and P-cycling SEAs was mainly attributable to the microbial stimulation by biochar properties (i.e., nutrient content and porosity) and soil nutrients (e.g., soil organic C and total N). The enhancement was the most significant under the conditions with biochars produced at low temperatures and using feedstock materials with high nutrient content, and biochar applications in acidic or neutral soils, coarse or fine soils, and farmland soils. Biochar additions to soils overall reduced the C-cycling SEAs by 6.3%. The C-cycling SEAs were greatly suppressed under the conditions with low and very high biochar loads, biochars produced at high temperatures and with feedstock materials of herb and lignocellulose, and biochar applications in alkaline, fine, and forest soils. The results were mainly related to the adsorption and inhibition effects of biochars and soil properties (e.g., liming effect, high biochar porosity and aromatic C content) on fungi and the enzymes. Biochar feedstock, C/N and load, and soil total N were the main influential factors on the SEAs. The results from this study demonstrate that biochar amendment is beneficial to improving soil N and P cycling and C sequestration.
机译:该荟萃分析的目的是综合生物炭修正对与碳(C),氮(N)和磷(P)循环相关的土壤酶活性(海)的影响。基于401个配对比较,从43名发布的研究,响应于生物炭特征,土壤性质和实验条件,分析了海洋和主要影响因素。结果表明,生物炭加入土壤,总体增加了N-和P循环海洋的增加14%和11%。 N-和P循环海域的增强主要是由生物炭特性(即营养含量和孔隙率)和土壤营养素(例如土壤有机C和总N)的微生物刺激。该增强在低温下产生的生物触体和使用具有高营养含量的原料材料,以及酸性或中性土壤,粗糙或细土壤以及农田土壤的生物炭应用,增强是最重要的。生物炭加入土壤总体减少了C循环海洋6.3%。在具有低和非常高的生物炭载荷的条件下大大抑制了C循环海洋,在高温下生产的生物炸药物以及草本植物和木质纤维素的原料材料,以及碱性,精细和森林土壤的生物炭应用。结果主要涉及生物触发和土壤性质的吸附和抑制作用(例如,估计效应,高生物施孔隙率和芳香C含量)对真菌和酶。生物炭原料,C / N和负荷,土壤总体N是海洋的主要影响因素。本研究结果表明,生物炭修正案有利于改善土壤n和p循环和c螯合。

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