Do phosphorus amendments enhance biodegradation activity in stalled petroleum hydrocarbon-contaminated soil?

IF 2.2 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES Journal of environmental quality Pub Date : 2024-07-12 DOI:10.1002/jeq2.20594
Aimée D. Schryer, Steven D. Siciliano
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Abstract

Phosphorus (P) fertilizers promote soil petroleum-hydrocarbon (PHC) bioremediation by correcting carbon-to-P ratio imbalances. While these inputs create conditions favorable to microbial growth, areas of a site or an entire site with low degradation rates (i.e., “stalled”) occur for unknown reasons. We hypothesized that soil conditions limit P bioavailability, leading to stalls in PHC bioremediation, and adding the correct P amendment restarts microbial activity. Soils were collected and characterized from four cold calcareous PHC-impacted sites in Saskatchewan, Canada, undergoing bioremediation. A generalized linear mixed model identified that regions with lower degradation rates possessed a neutral pH with high magnetic and salinity values. In a subsequent laboratory experiment, the proportion of benzene degraded at greater rates within active (i.e., higher degradation rates) than stalled soils, thereby following model predictions (p-value = 0.19, Kruskal–Wallis). The PHC degradation efficiency of different P amendments was tested by doping stalled soils (n = 3) with one of five treatments: 0 (control), 0 (autoclaved control), or 50 mg phosphate kg−1 soil as sodium diphosphate, triethyl phosphate, or tripolyphosphate. Tripolyphosphate accelerated benzene degradation (75.5 ± 5.4%) in one stalled soil (Outlook 323) and increased degradation non-significantly (43.9 ± 9.4%) in another (Allan 917). Alternatively, the final sample (Davidson 421) possessed the greatest benzene removal with no amendments. This implies that soil P bioavailability may not be the sole cause of decreased microbial activity. Accordingly, combining model outputs with mineralogy and microbiology investigations could enhance PHC biodegradation rates in these cold calcareous soils.

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磷添加剂是否能增强受石油烃污染的停滞土壤中的生物降解活性?
磷(P)肥通过纠正碳-磷比例失调,促进土壤石油烃(PHC)的生物修复。虽然这些投入创造了有利于微生物生长的条件,但还是会出现降解率低(即 "停滞")的区域或整个场地,原因不明。我们假设,土壤条件限制了钾的生物利用率,导致 PHC 生物修复停滞,而添加正确的钾添加剂则可重新启动微生物活动。我们从加拿大萨斯喀彻温省四个受冷钙质 PHC 影响、正在进行生物修复的地点收集了土壤,并对其进行了特征描述。通过广义线性混合模型发现,降解率较低的地区 pH 值呈中性,磁性和盐度值较高。在随后的实验室实验中,活跃土壤(即降解率较高)中苯的降解率高于停滞土壤,因此符合模型预测(P 值 = 0.19,Kruskal-Wallis)。通过在停滞土壤(n = 3)中掺入五种处理之一,测试了不同 PHC 添加剂的 PHC 降解效率:0(对照)、0(高压灭菌对照)或 50 毫克磷酸盐 kg-1 土壤(二磷酸钠、磷酸三乙酯或三聚磷酸钠)。在一种停滞的土壤(Outlook 323)中,三聚磷酸钠加速了苯(75.5 ± 5.4%)的降解,而在另一种土壤(Allan 917)中,三聚磷酸钠无显著性地增加了降解(43.9 ± 9.4%)。另外,最终样本(Davidson 421)在不添加任何添加剂的情况下苯去除率最高。这意味着土壤中 P 的生物利用率可能不是微生物活性降低的唯一原因。因此,将模型输出与矿物学和微生物学调查相结合,可以提高这些寒冷石灰性土壤中 PHC 的生物降解率。
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来源期刊
Journal of environmental quality
Journal of environmental quality 环境科学-环境科学
CiteScore
4.90
自引率
8.30%
发文量
123
审稿时长
3 months
期刊介绍: Articles in JEQ cover various aspects of anthropogenic impacts on the environment, including agricultural, terrestrial, atmospheric, and aquatic systems, with emphasis on the understanding of underlying processes. To be acceptable for consideration in JEQ, a manuscript must make a significant contribution to the advancement of knowledge or toward a better understanding of existing concepts. The study should define principles of broad applicability, be related to problems over a sizable geographic area, or be of potential interest to a representative number of scientists. Emphasis is given to the understanding of underlying processes rather than to monitoring. Contributions are accepted from all disciplines for consideration by the editorial board. Manuscripts may be volunteered, invited, or coordinated as a special section or symposium.
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