Mineralization of microalgal carbon and nitrogen in sodic soils

Ileana Castro-González, Héctor Iván Bedolla-Rivera, M. Negrete-Rodríguez, Omar S. Castillo, D. Álvarez-Bernal, E. Conde-Barajas
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Abstract

Sodic soils pose a challenge for the agricultural production due to their lack of nutrients, poor structure, low organic matter content, and susceptibility to erosion (water and wind). Their recovery is carried out by soil washing and applying calcium salts, which are sometimes unprofitable processes. A low-cost and environmentally friendly alternative to remedy adverse soil conditions is bioremediation using microorganisms or organic amendments. For this reason, this study intended to evaluate the effects of the addition of dry microalgal biomass on sodic soils and suggest its use as an organic amendment. The effect of the microalgal biomass was studied through the mineralization dynamics of carbon and nitrogen sources in short-term experiments. All experiments were performed at laboratory scale. Microalgal biomass was obtained from a consortium grown in dairy wastewater and subsequently dried and pulverized. Four different treatments of dry microalgal biomass were applied to 50 g of sodic soil, and high microbial activity was observed in the soil (obtaining a production of 240 mg C-CO2/kg dry soil), along with the production of nitrates (presenting values 33.8-1.45 mg N-NO3+/kg dry soil) via the release of ammonia (obtaining 5.46 mg N-NH3+/kg dry soil), and mineralization of organic N into ammonium (producing 1071.92 mg N-NH4+/kg dry soil). The microalgal biomass as an organic amendment showed to be prone to mineralization and release of carbon and nitrogen sources, improving the microbial activity in a soil with sodicity problems.
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钠质土壤中微型藻类碳和氮的矿化
钠盐土壤由于缺乏养分、结构不良、有机质含量低以及易受侵蚀(水和风),给农业生产带来了挑战。恢复土壤的方法是冲洗土壤和施用钙盐,但这些方法有时无利可图。利用微生物或有机添加剂进行生物修复是一种低成本、环保的土壤修复方法。因此,本研究旨在评估添加干燥微藻生物质对钠盐土壤的影响,并建议将其用作有机改良剂。在短期实验中,通过碳源和氮源的矿化动态研究了微藻生物质的效果。所有实验均在实验室规模下进行。微藻生物质来自一个在乳制品废水中生长的联合体,随后进行干燥和粉碎。在 50 克含钠土壤中施用了四种不同处理的干微藻生物质,观察到土壤中微生物活性很高(产生 240 毫克 C-CO2/千克干土),同时通过释放氨(产生 5.46 毫克 N-NH3+/千克干土)产生硝酸盐(产生 33.8-1.45 毫克 N-NO3+/千克干土),并将有机氮矿化为铵(产生 1071.92 毫克 N-NH4+/千克干土)。微藻生物质作为一种有机改良剂,容易矿化并释放碳源和氮源,从而改善有钠化问题的土壤中的微生物活性。
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