Total and labile carbon and nitrogen in anthropogenic and native soils of New York City

Kohinoor Begum, Zhongqi Cheng, Geraldine N. Vega Pizarro, Milton E. Vega Luna, Braden Fleming, Austin Price, Joxelle Velázquez García, Randy Riddle, Donald C. Parizek, Luis A. Hernandez, Richard K. Shaw, Peter M. Groffman
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Abstract

Urban soils are key components of urban ecosystems and can contribute to the solution for many ecological and environmental problems such as stormwater runoff, pollution mitigation, and urban food production. Urbanization processes often result in highly disturbed and spatially variable urban soils. Besides heterogeneity, one of the unique and intriguing aspects of urban soil is the nature and properties of organic carbon, with a significant percentage being anthropogenic carbon such as black carbon, which is less biologically active than natural organic matter. We sampled 13 soil profiles covering a wide range of soil conditions, including both anthropogenic and native soils, across New York City. At each site from each horizon, soil samples were collected for laboratory determination of total carbon and nitrogen, black carbon, microbial biomass carbon and nitrogen, and pools of readily mineralizable carbon and nitrogen. We hypothesized that the carbon present in urban soil profiles derived from human-altered and human-transported (HAHT) parent materials has a lower capacity to support microbial biomass and a limited nitrogen supplying ability compared to the carbon found in urban soils derived from native parent materials. We found that total carbon and nitrogen were as high, or even higher in soils derived from HAHT parent materials than in native soil profiles, but that labile pools were lower in the HAHT soils. Assessment of the quality of organic carbon, which is strongly affected by HAHT materials, is important for understanding the ability of urban soils to support a wide range of ecological and environmental functions.

Abstract Image

Abstract Image

纽约市人为土壤和天然土壤的总碳和活性氮
城市土壤是城市生态系统的关键组成部分,有助于解决许多生态和环境问题,如雨水径流、污染缓解和城市粮食生产。城市化进程往往导致城市土壤受到高度干扰和空间变化。除了异质性之外,城市土壤的一个独特而有趣的方面是有机碳的性质和特性,其中很大一部分是人为碳,如黑碳,其生物活性低于天然有机质。我们在纽约市采样了13个土壤剖面,涵盖了广泛的土壤条件,包括人为土壤和天然土壤。在每个地点,从每个层位收集土壤样品,用于实验室测定总碳和氮、黑碳、微生物生物量碳和氮以及易矿化碳和氮池。我们假设,与来自原生母质的城市土壤中的碳相比,来自人为改变和人为运输(HAHT)母质的城市土壤剖面中的碳支持微生物生物量的能力较低,氮供应能力有限。我们发现,与天然土壤剖面相比,高温母质土壤的总碳和总氮同样高,甚至更高,但在高温土壤中,不稳定库的含量较低。有机碳的质量受到高温材料的强烈影响,对了解城市土壤支持各种生态和环境功能的能力具有重要意义。
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