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土壤生物地球化学对多种人类引起的环境变化共同作用的响应。

Soil biogeochemical responses to multiple co-occurring forms of human-induced environmental change.

机构信息

School of Mathematical and Natural Sciences, Arizona State University at the West Campus, 1407 W. Thunderbird Rd., Glendale, AZ, 85306, USA.

出版信息

Oecologia. 2023 Apr;201(4):1109-1121. doi: 10.1007/s00442-023-05360-7. Epub 2023 Mar 16.

Abstract

Human activities cause a multitude of environmental issues, including increased temperatures and altered precipitation patterns associated with climate change, air pollution, and other impacts of urbanization. One area highly affected by these issues is the Sonoran Desert, specifically the Phoenix metropolitan area where urbanization is among the most rapid in the United States. Most studies investigate these multiple environmental change factors independently or sometimes in pairs, but rarely all together as co-occurring forms of change. We examined how the simultaneous manipulation of increasing temperatures, altered precipitation patterns, nitrogen deposition, and urbanization influenced soil respiration and mineral N pools in the Sonoran Desert. Soil was collected from urban and exurban sites, from both nitrogen-fertilized and control plots. To simulate projected climate change, the soils were incubated in microcosm at the annual average Phoenix temperature as well a 2 ℃ increase under a factorial precipitation treatment of decreased frequency and increased pulse size. Our results show that C and N dynamics were altered by all four forms of environmental change. However, the dominance of significant 3- and 4-way interactions among the four environmental factors for both respiration and mineral N pools demonstrates that the impact of any given form of environmental change will depend on the levels of the other environmental factors. In other words, the cumulative effect of altered precipitation, fertilization, temperature, and urbanization on soil biogeochemical processes is not necessarily predictable from their individual impact.

摘要

人类活动导致了许多环境问题,包括与气候变化、空气污染和城市化其他影响相关的气温升高和降水模式改变。受这些问题影响最严重的地区之一是索诺兰沙漠,特别是凤凰城大都市区,那里的城市化速度是美国最快的。大多数研究独立地或有时成对地研究这些多种环境变化因素,但很少将它们作为同时发生的变化形式一起研究。我们研究了气温升高、降水模式改变、氮沉积和城市化的同时作用如何影响索诺兰沙漠的土壤呼吸和矿质氮库。我们从城市和远郊地区、施肥和对照小区采集了土壤样本。为了模拟预期的气候变化,我们在微生境中培养土壤,温度为凤凰城的年平均温度,在降水处理下增加 2°C,该处理减少了降水频率,增加了脉冲大小。我们的结果表明,所有四种形式的环境变化都改变了 C 和 N 的动态。然而,对于呼吸和矿质 N 库,四个环境因素之间的显著 3 路和 4 路相互作用占主导地位,这表明任何给定形式的环境变化的影响将取决于其他环境因素的水平。换句话说,降水、施肥、温度和城市化改变对土壤生物地球化学过程的累积影响不一定可以从它们各自的影响中预测。

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