Long-term fertilization increases soil but not plant or microbial N in a Chihuahuan Desert grassland

Violeta Mendoza-Martinez, S. Collins, Jennie R. McLaren
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Abstract

Abstract. Although the negative consequences of increased nitrogen (N) supply for plant communities and soil chemistry are well known, most studies have focused on mesic grasslands, and the fate of added N in arid and semi-arid ecosystems remains unclear. To study the impacts of long-term increased N deposition on ecosystem N pools, we sampled a 26-year-long fertilization (10 g N m−2 yr−1) experiment in the northern Chihuahuan Desert at the Sevilleta National Wildlife Refuge (SNWR) in New Mexico. To determine the fate of the added N, we measured multiple soil, microbial, and plant N pools in shallow soils at three time points across the 2020 growing season. We found small but significant increases with fertilization in soil-available NO3--N and NH4+-N, yet the soil microbial and plant communities do not appear to be taking advantage of the increased N availability, with no changes in biomass or N content in either community. However, there were increases in total soil N with fertilization, suggesting increases in microbial or plant N earlier in the experiment. Ultimately, the majority of the N added in this multi-decadal experiment was not found in the shallow soil or the microbial or plant community and is likely to have been lost from the ecosystem entirely.
在奇瓦瓦沙漠草地上,长期施肥会增加土壤中的氮含量,但不会增加植物或微生物的氮含量
摘要虽然氮(N)供应增加对植物群落和土壤化学的负面影响已众所周知,但大多数研究都集中在中生代草地上,而增加的氮在干旱和半干旱生态系统中的归宿仍不清楚。为了研究长期增加的氮沉积对生态系统氮库的影响,我们在新墨西哥州塞维莱塔国家野生动物保护区(SNWR)的奇瓦瓦沙漠北部进行了长达 26 年的施肥(10 克氮 m-2 yr-1)实验取样。为了确定添加的氮的去向,我们在 2020 年生长季节的三个时间点测量了浅层土壤中的多个土壤、微生物和植物氮库。我们发现,施肥后,土壤中可利用的 NO3-N 和 NH4+-N 虽有少量增加,但效果显著,而土壤微生物群落和植物群落似乎并没有利用增加的氮,这两个群落的生物量或氮含量都没有发生变化。不过,施肥后土壤中的总氮有所增加,这表明在实验早期微生物或植物的氮有所增加。最终,在这项长达数十年的实验中,大部分增加的氮并没有出现在浅层土壤或微生物或植物群落中,很可能已经从生态系统中完全流失了。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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