dc.creatorLiptzin, D.
dc.creatorRieke, E.L.
dc.creatorCappellazzi, S.B.
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dc.creatorGreub, K.L.H.
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dc.creatorBañuelos, O.
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dc.creatorBaumhardt, R.L.
dc.creatorBorbón Gracia, A.
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dc.creatorCarlyle, C.N.
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dc.creatorSandeep Kumar
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dc.creatorPonce Lira, B.
dc.creatorReeve, J.R.
dc.creatorReinbott, T.M.
dc.creatorReiter, M.S.
dc.creatorRitchey, E.L.
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dc.creatorYichao Rui
dc.creatorSadeghpour, A.
dc.creatorSainju, U.M.
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dc.creatorSchillinger, W.F.
dc.creatorSchindelbeck, R.R.
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dc.creatorSykes, V.R.
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dc.creatorVan Es, H.M.
dc.creatorVerhulst, N.
dc.creatorVyn, T.J.
dc.creatorYutao Wang
dc.creatorWatts, D.B.
dc.creatorWright, D.L.
dc.creatorTiequan Zhang
dc.creatorMorgan, C.L.S.
dc.creatorHoneycutt, C.W.
dc.date2023-07-05T20:30:12Z
dc.date2023-07-05T20:30:12Z
dc.date2023
dc.date.accessioned2023-07-17T20:10:42Z
dc.date.available2023-07-17T20:10:42Z
dc.identifierhttps://hdl.handle.net/10883/22639
dc.identifier10.1002/saj2.20558
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/7514381
dc.descriptionVarious soil health indicators that measure a chemically defined fraction of nitrogen (N) or a process related to N cycling have been proposed to quantify the potential to supply N to crops, a key soil function. We evaluated five N indicators (total soil N, autoclavable citrate extractable N, water-extractable organic N, potentially mineralizable N, and N-acetyl-β-D-glucosaminidase activity) at 124 sites with long-term experiments across North America evaluating a variety of managements. We found that 59%–81% of the variation in N indicators was among sites, with indicator values decreasing with temperature and increasing with precipitation and clay content. The N indicators increased from 6%–39% in response to decreasing tillage, cover cropping, retaining residue, and applying organic sources of nutrients. Overall, increasing the quantity of organic inputs, whether from increased residue retention, cover cropping, or rotations with higher biomass, resulted in higher values of the N indicators. Although N indicators responded to management in similar ways, the analysis cost and availability of testing laboratories is highly variable. Further, given the strong relationships of the N indicators with carbon (C) indicators, measuring soil organic C along with 24-h potential C mineralization could be used as a proxy for N supply instead of measuring potentially mineralizable N or any other N indicator directly.
dc.languageEnglish
dc.publisherJohn Wiley & Sons Inc.
dc.rightsCIMMYT manages Intellectual Assets as International Public Goods. The user is free to download, print, store and share this work. In case you want to translate or create any other derivative work and share or distribute such translation/derivative work, please contact CIMMYT-Knowledge-Center@cgiar.org indicating the work you want to use and the kind of use you intend; CIMMYT will contact you with the suitable license for that purpose
dc.rightsOpen Access
dc.sourceIn press
dc.source0361-5995
dc.sourceSoil Science Society of America Journal
dc.subjectAGRICULTURAL SCIENCES AND BIOTECHNOLOGY
dc.subjectSoil Health Indicators
dc.subjectNitrogen Fraction
dc.subjectCarbon and Nitrogen Indicators
dc.subjectCarbon Mineralization Potential
dc.subjectNITROGEN
dc.subjectSOIL QUALITY
dc.subjectLONG TERM EXPERIMENTS
dc.subjectCROP YIELD
dc.subjectSustainable Agrifood Systems
dc.titleAn evaluation of nitrogen indicators for soil health in long-term agricultural experiments
dc.typeArticle
dc.typePublished Version
dc.coverageMadison, WI (USA)


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