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Humic substances cycling in a tropical oxbow lagoon (Sao Paulo, Brazil)

机译:腐殖质在热带牛弓泻湖中循环(巴西圣保罗)

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摘要

This study aimed at describing the cycling of humic substances (HS) in a tropical oxbow lagoon (Sao Paulo, Brazil). Humic substances were obtained from Oxycaryum cubense leachate submitted to degradation and fractionated into fulvic acid (FA) and humic acid (HA). Incubations were prepared using FA and HA and water from Infernao lagoon and maintained under high dissolved oxygen (HDO) and low dissolved oxygen (LDO) conditions at 16 degrees C, 22 degrees C and 26 degrees C. FA and HA decay was monitored (on a carbon basis) for 40 days. The results were fitted to first-order kinetics model and the effect of temperature and oxygen availability on mineralization of FA and HA was described and used on simulations of humic substance cycling. The simulations allowed us to infer that in the Infernao lagoon HS mineralization is faster under LDO than under HDO conditions, with higher mineralization occurring in February (summer) and HA presented lower mineralization coefficients. For the Infernao lagoon, HS decay is a slow process and these compounds are expected to be extensively incorporated into the sediments of this environment. (C) 2007 Elsevier Ltd. All rights reserved.
机译:这项研究的目的是描述热带牛棚泻湖(巴西圣保罗)中腐殖质(HS)的循环。腐殖质是从立方丁酸草浸出液中降解得到的,并分为黄腐酸(FA)和腐殖酸(HA)。使用FA和HA以及来自Infernao泻湖的水制备培养物,并在16°C,22°C和26°C下保持在高溶解氧(HDO)和低溶解氧(LDO)条件下。监测FA和HA的衰减以碳为基础)持续40天。结果适合一阶动力学模型,描述了温度和氧气利用率对FA和HA矿化的影响,并将其用于腐殖质循环的模拟。通过模拟可以推断出,在Infernao泻湖中,LDO下的HS矿化比HDO下的更快,在2月(夏季)发生更高的矿化,而HA的矿化系数更低。对于Infernao泻湖,HS衰减是一个缓慢的过程,预计这些化合物将广泛地掺入该环境的沉积物中。 (C)2007 Elsevier Ltd.保留所有权利。

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