30年的降水量增加改变了中部草原的土壤有机质组分,但没有改变土壤的整体碳和氮

IF 9.8 1区 农林科学 Q1 SOIL SCIENCE Soil Biology & Biochemistry Pub Date : 2023-10-01 DOI:10.1016/j.soilbio.2023.109145
Katherine S. Rocci , Michael Bird , John M. Blair , Alan K. Knapp , Chao Liang , M. Francesca Cotrufo
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引用次数: 0

摘要

众所周知,对气候变化敏感的草地生态系统显示,尽管植物和土壤微生物的湿度引起变化(例如,土壤C和N的预期驱动因素),土壤碳(C)和氮(N)库对增加的水分有效性的响应最小。然而,尚不清楚这种明显的有限响应是由于地下系统的不响应,还是由于多种土壤有机质(SOM)组分库和通量的变化相互抵消。为了研究SOM中C和N对年代际降水增加的潜在响应,我们在一个每年被烧毁的中型草地上进行了30年的降水增加试验。我们测量了三种不同植物和微生物对照的SOM组分中的C和N: 1)自由颗粒OM (fPOM), 2)封闭POM加重粗OM (oPOM + hcOM), 3)矿物相关OM (MAOM),以及氨基糖,热原C和N,和根质量指标。我们发现,随着降水的增加,体积C和N没有变化,但SOM组分发生了变化。植物投入和土壤氮有效性的改变驱动了fPOM N和oPOM + hcOM C:N的响应,它们分别随着降水的增加而增加和减少。相比之下,在降水增加下观测到的MAOM C和N的增加可能与特定的驱动因素无关,这表明可能需要额外的植物、微生物或矿物测量。无论如何,我们的研究结果表明,与仅测量大块SOM相比,调查SOM组分可能更直接地联系土壤C和N库及其驱动因素。此外,我们发现在降水增加的情况下,土壤C储存可能随着水分有效性的增加而对气候变化提供负反馈,但缺乏总体SOM响应表明这种反馈在mesic草原不强。
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Thirty years of increased precipitation modifies soil organic matter fractions but not bulk soil carbon and nitrogen in a mesic grassland

Grassland ecosystems, which are known to be sensitive to climate change, have shown minimal responses of soil carbon (C) and nitrogen (N) pools to increased moisture availability, despite moisture-induced changes in plants and soil microbes (e.g., expected drivers of soil C and N). However, it is not clear if this apparent limited response is due to an unresponsive belowground system or because alterations in multiple soil organic matter (SOM) component pools and fluxes offset each other. To investigate potential responses of C and N in SOM to decadal increases in precipitation, we sampled soils from a 30-year precipitation augmentation experiment in an annually burned mesic grassland. We measured C and N in three SOM fractions which vary in their plant and microbial controls 1) free particulate OM (fPOM), 2) occluded POM plus heavy, coarse OM (oPOM + hcOM), and 3) mineral-associated OM (MAOM), as well as amino sugars, pyrogenic C and N, and root quality metrics. We found no changes in bulk C or N under increased precipitation, but SOM fractions were modified. Altered plant inputs and soil N availability appeared to drive the responses of fPOM N and oPOM + hcOM C:N, which were increased and decreased, respectively, by increased precipitation. In contrast, the observed increase in MAOM C and N under increased precipitation could not be connected to a specific driver, suggesting additional plant, microbial, or mineral measurements may be required. Regardless, our results indicate that investigating SOM fractions may more directly connect soil C and N pools and their drivers, compared to measuring only bulk SOM. Further, our finding of greater stable OM (MAOM) under increased precipitation suggests soil C storage could provide a negative feedback to climate change with increased moisture availability, but the lack of bulk SOM response suggests that this feedback is not strong in mesic grasslands.

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来源期刊
Soil Biology & Biochemistry
Soil Biology & Biochemistry 农林科学-土壤科学
CiteScore
16.90
自引率
9.30%
发文量
312
审稿时长
49 days
期刊介绍: Soil Biology & Biochemistry publishes original research articles of international significance focusing on biological processes in soil and their applications to soil and environmental quality. Major topics include the ecology and biochemical processes of soil organisms, their effects on the environment, and interactions with plants. The journal also welcomes state-of-the-art reviews and discussions on contemporary research in soil biology and biochemistry.
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