{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,4]],"date-time":"2026-04-04T18:29:27Z","timestamp":1775327367574,"version":"3.50.1"},"reference-count":137,"publisher":"MDPI AG","issue":"18","license":[{"start":{"date-parts":[[2023,9,12]],"date-time":"2023-09-12T00:00:00Z","timestamp":1694476800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"framework of state assignment","award":["FGUR-2022-0009"],"award-info":[{"award-number":["FGUR-2022-0009"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>For most of the arable land in Russia (132\u2013137 million ha), the dominant and accurate soil information is stored in the form of map archives on paper without coordinate reference. The last traditional soil map(s) (TSM, TSMs) were created over 30 years ago. Traditional and\/or archival soil map(s) (ASM, ASMs) are outdated in terms of storage formats, dates, and methods of production. The technology of constructing a multitemporal soil line (MSL) makes it possible to update ASMs and TSMs based on the processing of big remote-sensing data (RSD). To construct an MSL, the spectral characteristics of the bare soil surface (BSS) are used. The BSS on RSD is distinguished within the framework of the conceptual apparatus of the spectral neighborhood of the soil line. The filtering of big RSD is based on deep machine learning. In the course of the work, a vector georeferenced version of the ASM and an updated soil map were created based on the coefficient \u201cC\u201d of the MSL. The maps were verified based on field surveys (76 soil pits). The updated map is called the map of soil interpretation of the coefficient \u201cC\u201d (SIC \u201cC\u201d). The SIC \u201cC\u201d map has a more detailed legend compared to the ASM (7 sections\/chapters instead of 5), greater accuracy (smaller errors of the first and second kind), and potential suitability for calculating soil organic matter\/carbon (SOM\/SOC) reserves (soil types\/areals in the SIC \u201cC\u201d map are statistically significant are divided according to the thickness of the organomineral horizon and the content of SOM in the plowed layer). When updating, a systematic underestimation of the numbers of contours and areas of soils with manifestations of negative\/degradation soil processes (slitization and erosion) on the TSM was established. In the process of updating, all three shortcomings of the ASMs\/TSMs (archaic storage, dates, and methods of creation) were eliminated. The SIC \u201cC\u201d map is digital (thematic raster), modern, and created based on big data processing methods. For the first time, the actualization of the soil map was carried out based on the MSL characteristics (coefficient \u201cC\u201d).<\/jats:p>","DOI":"10.3390\/rs15184491","type":"journal-article","created":{"date-parts":[[2023,9,12]],"date-time":"2023-09-12T21:41:12Z","timestamp":1694554872000},"page":"4491","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":12,"title":["Updating of the Archival Large-Scale Soil Map Based on the Multitemporal Spectral Characteristics of the Bare Soil Surface Landsat Scenes"],"prefix":"10.3390","volume":"15","author":[{"given":"Dmitry I.","family":"Rukhovich","sequence":"first","affiliation":[{"name":"V.V. Dokuchaev Soil Science Institute, Pyzhevskiy Pereulok 7, 119017 Moscow, Russia"}]},{"given":"Polina V.","family":"Koroleva","sequence":"additional","affiliation":[{"name":"V.V. Dokuchaev Soil Science Institute, Pyzhevskiy Pereulok 7, 119017 Moscow, Russia"}]},{"given":"Alexey D.","family":"Rukhovich","sequence":"additional","affiliation":[{"name":"V.V. Dokuchaev Soil Science Institute, Pyzhevskiy Pereulok 7, 119017 Moscow, Russia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6135-7212","authenticated-orcid":false,"given":"Mikhail A.","family":"Komissarov","sequence":"additional","affiliation":[{"name":"Ufa Institute of Biology UFRC RAS, Pr. Oktyabrya 69, 450054 Ufa, Russia"}]}],"member":"1968","published-online":{"date-parts":[[2023,9,12]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"35","DOI":"10.1016\/0016-7061(74)90036-6","article-title":"Structure of the soil mantle","volume":"12","author":"Fridland","year":"1974","journal-title":"Geoderma"},{"key":"ref_2","unstructured":"Fridland, V.M. (1977). 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