{"refrec":{"BRefID":352865,"RR":"<b>Sulpis, O.; Humphreys, M.P.; Wilhelmus, M.M.; Carroll, D.; Berelson, W.M.; Menemenlis, D.; Middelburg, J.J.; Adkins, J.F.</b> (2022). RADIv1: a non-steady-state early diagenetic model for ocean sediments in Julia and MATLAB/GNU Octave. <i>Geosci. Model Dev. 15(5)</i>: 2105-2131. <a href=\"https://dx.doi.org/10.5194/gmd-15-2105-2022\" target=\"_blank\">https://dx.doi.org/10.5194/gmd-15-2105-2022</a>","BEntID":350574,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geosci. Model Dev. 15(5)</i>: 2105-2131. <a href=\"https://dx.doi.org/10.5194/gmd-15-2105-2022\" target=\"_blank\">https://dx.doi.org/10.5194/gmd-15-2105-2022</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Sulpis, O.; Humphreys, M.P.; Wilhelmus, M.M.; Carroll, D.; Berelson, W.M.; Menemenlis, D.; Middelburg, J.J.; Adkins, J.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Sulpis, O. <i>et al.</i>","Englishabstract":"We introduce a time-dependent, one-dimensional model of early diagenesis    that we term RADI, an acronym accounting for the main processes included in    the model: chemical reactions, advection, molecular and bio-diffusion, and    bio-irrigation. RADI is targeted for study of deep-sea sediments, in    particular those containing calcium carbonates (CaCO<sub>3</sub>). RADI    combines CaCO<sub>3</sub> dissolution driven by organic matter degradation    with a diffusive boundary layer and integrates state-of-the-art    parameterizations of CaCO<sub>3</sub> dissolution kinetics in seawater,    thus serving as a link between mechanistic surface reaction modeling and    global-scale biogeochemical models. RADI also includes CaCO<sub>3</sub>    precipitation, providing a continuum between CaCO<sub>3</sub> dissolution    and precipitation. RADI integrates components rather than individual    chemical species for accessibility and is straightforward to compare    against measurements. RADI is the first diagenetic model implemented in    Julia, a high-performance programming language that is free and open    source, and it is also available in MATLAB/GNU Octave. Here, we first    describe the scientific background behind RADI and its implementations.    Following this, we evaluate its performance in three selected locations and    explore other potential applications, such as the influence of tides and    seasonality on early diagenesis in the deep ocean. RADI is a powerful tool    to study the time-transient and steady-state response of the sedimentary    system to environmental perturbation, such as deep-sea mining,    deoxygenation, or acidification events.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"RADIv1: a non-steady-state early diagenetic model for ocean sediments in Julia and MATLAB/GNU Octave","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-20 01:32:51.094515","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-06-22","DateCreate":"2022-06-22","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000769796000001","VABBcode":null,"OpenAcc":1,"DOI":"10.5194/gmd-15-2105-2022"},"refs":null,"anarec":{"AnaID":352865,"PubliDate":2022,"Pagination":"2105-2131","XtraPublOfAnaID":null,"ISBN":null,"Volume":"15","Issue":"5","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":209852,"SerRR":"Geoscientific Model Development. Copernicus Publications: Göttingen.  ISSN 1991-959X; e-ISSN 1991-9603","StandardTitleSer":"Geoscientific Model Development","ISSN":"1991-959X","AbbrevSer":"Geosci. 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