生物炭与有机废弃物复合对土壤化学性质和植物生长影响不大

IF 2 Q3 SOIL SCIENCE
M. Rodrigues, Tais Garmus, M. Arrobas, A. Gonçalves, Ermelinda Silva, Luis Mateus Rocha, Luís Pinto, Cátia Brito, Sandra Martins, T. Vargas, C. Correia
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引用次数: 6

摘要

生物炭作为一种土壤调理剂受到了极大的关注,因为它可以潜在地螯合土壤中的碳,增强土壤的物理、化学和生物特性,提高作物生产力。本研究报告了橄榄(Olea europaea L.)在酸性粘壤土中进行的盆栽试验结果,该试验在八种施肥处理下的两个生长季节进行。其中包括相当于100 kg ha-1的N、P2O5和K2O(NPK)的矿物肥料,以10(B10)和20(B20)t的速率施用生物炭ha-1,生物炭NPK混合物(B10+NPK),生物炭废物与蘑菇废物堆肥的混合物(B10+MWC),橄榄厂废物(B10+OMW)和城市固体废物(B10+MSW),有机材料以20 t ha-1的速率施用,以及不施肥的处理(对照)。与对照相比,B20处理中的生物炭增加了土壤碳含量。与NPK处理相比,B10+NPK处理中的生物炭降低了土壤硝酸盐水平。使用生物炭没有观察到对土壤性质、养分吸收或植物生长的其他益处,也没有观察到生物炭与其他有机改良剂的混合物有任何积极的协同作用。与对照相比,MSW、OMW和MWC倾向于增加土壤pH。大多数生物炭研究都是在土壤限制或恶劣环境条件限制植物生长的土壤中进行的,这可能有助于检测有利的影响。在限制较少的土壤或植物的压力条件下,例如本实验中建立的条件下,使用生物炭的好处很差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Combined biochar and organic waste have little effect on chemical soil properties and plant growth
Biochar has received great attention as a soil conditioner since it can potentially sequester carbon (C) in soil, enhance soil physical, chemical and biological properties and improve crop productivity. This study reports the results of a pot experiment with olive (Olea europaea L.), carried out in an acidic and clay loam textured soil, and cultivated during two growing seasons under eight fertilization treatments. They included mineral fertilization equivalent to a rate of 100 kg ha-1 of N, P2O5 and K2O (NPK), biochar applied at a rate of 10 (B10), and at 20 (B20) t biochar ha-1, biochar-NPK mixture (B10+NPK), biochar-waste mixtures with mushroom waste compost (B10+MWC), olive mill waste (B10 + OMW), and municipal solid waste (B10+MSW), the organic materials applied at a rate of 20 t ha-1, together with a treatment without fertilization (control). Biochar in the B20 treatment increased the soil C content in comparison to the control. Biochar in the B10+NPK treatment reduced soil nitrate levels compared to NPK treatment. No other benefits to soil properties, nutrient uptake or plant growth were observed with the use of biochar or any positive synergistic effect with the mixture of biochar with the other organic amendments. MSW, OMW and MWC tended to increase soil pH in comparison to the control. Most of the studies with biochar were carried out in soils with edaphic limitations or harsh environmental conditions limiting plant growth, which may have facilitated the detection of favorable effects. Under less limited soils or stressful conditions for plants, such as the ones established in this experiment, the benefits of using biochar were poor.
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来源期刊
CiteScore
2.20
自引率
0.00%
发文量
13
期刊介绍: The Spanish Journal of Soil Science (SJSS) is a peer-reviewed journal with open access for the publication of Soil Science research, which is published every four months. This publication welcomes works from all parts of the world and different geographic areas. It aims to publish original, innovative, and high-quality scientific papers related to field and laboratory research on all basic and applied aspects of Soil Science. The journal is also interested in interdisciplinary studies linked to soil research, short communications presenting new findings and applications, and invited state of art reviews. The journal focuses on all the different areas of Soil Science represented by the Spanish Society of Soil Science: soil genesis, morphology and micromorphology, physics, chemistry, biology, mineralogy, biochemistry and its functions, classification, survey, and soil information systems; soil fertility and plant nutrition, hydrology and geomorphology; soil evaluation and land use planning; soil protection and conservation; soil degradation and remediation; soil quality; soil-plant relationships; soils and land use change; sustainability of ecosystems; soils and environmental quality; methods of soil analysis; pedometrics; new techniques and soil education. Other fields with growing interest include: digital soil mapping, soil nanotechnology, the modelling of biological and biochemical processes, mechanisms and processes responsible for the mobilization and immobilization of nutrients, organic matter stabilization, biogeochemical nutrient cycles, the influence of climatic change on soil processes and soil-plant relationships, carbon sequestration, and the role of soils in climatic change and ecological and environmental processes.
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