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xmlns:xlink="http://www.w3.org/1999/xlink"><gmd:MD_DataIdentification><gmd:citation><gmd:CI_Citation><gmd:title xsi:type="gmd:PT_FreeText_PropertyType"><gco:CharacterString>Topsoil dilution by subsoil admixture had less impact on the SOC stock development than fertilizer form and soil erosion state</gco:CharacterString><gmd:PT_FreeText><gmd:textGroup><gmd:LocalisedCharacterString locale="ger"> Die Verd&#252;nnung des Oberbodens durch Unterbodenbeimischung hatte weniger Einfluss auf die Entwicklung des SOC-Bestands als die D&#252;ngerform und der Zustand der Bodenerosion</gmd:LocalisedCharacterString></gmd:textGroup></gmd:PT_FreeText></gmd:title><gmd:alternateTitle><gco:CharacterString>Data collection: Part 0/5, table: Index</gco:CharacterString></gmd:alternateTitle><gmd:date><gmd:CI_Date><gmd:date><gco:Date>2024-03-27</gco:Date></gmd:date><gmd:dateType><CI_DateTypeCode xmlns="http://www.isotc211.org/2005/gmd" 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function for climate mitigation faced challenges, particularly with traditional measures having limited suitability for increasing soil organic carbon (SOC) stocks.  One way out of this dilemma could be to create an additional stable soil C sink by inducing SOC under saturation in the topsoil. In the past, attempts were made by abrupt topsoil dilution through subsoil admixture by means of deep tillage but with varying degrees of success. This was partly due to a lack of knowledge about the impact of soil condition like erosion state and N fertilization form ensuring optimum C input into the soil on the desired additional SOC accumulation and partly due to the lack of suitable experimental approaches to record the effect of all relevant factors simultaneously. To help solve these problems, a three-factorial experimental field trial were established: I.) "moderate topsoil dilution" (diluted vs non-diluted), II.) "N fertilization form" (mineral, i.e., calcium ammonium nitrate and urea vs organic, i.e., digestate) and III.)  "soil types" (Calcic Luvisol, Nudiargic Luvisol, and Calcaric Regosol) covering the typical range of erosion states in the hummocky ground moraine landscape of NE Germany. 
This datasets contains weather data, NDVI/RVI measurements data , soil texture data, soil and plant analysis data, CO2 flux obtained using a novel robotic chamber system that were conducted from 23.07.2020 (after manipulation) - 29.06.2021 (Harvest).

This table contains the index of all tables forming this data collection.

Related datasets are listed in the metadata element 'Related Identifier'.
Dataset version 1.0</gco:CharacterString><gmd:PT_FreeText><gmd:textGroup><gmd:LocalisedCharacterString locale="ger">Die derzeitigen Bem&#252;hungen, die Kohlenstoffsenkenfunktion von Agrar&#246;kosystemen f&#252;r den Klimaschutz zu verbessern, stehen vor Herausforderungen, insbesondere weil herk&#246;mmliche Ma&#223;nahmen nur begrenzt geeignet sind, den Bestand an organischem Kohlenstoff (SOC) im Boden zu erh&#246;hen.  Ein Ausweg aus diesem Dilemma k&#246;nnte darin bestehen, eine zus&#228;tzliche stabile C-Senke im Boden zu schaffen, indem der SOC im Oberboden in eine Unters&#228;ttigung gebracht wird. In der Vergangenheit wurden Versuche durch abrupte Verd&#252;nnung des Oberbodens durch Unterbodenbeimischung mittels tiefer Bodenbearbeitung unternommen, jedoch mit unterschiedlichem Erfolg. Dies lag zum einen an der mangelnden Kenntnis &#252;ber den Einfluss der Bodenbeschaffenheit wie Erosionszustand und N-D&#252;ngungsform, die einen optimalen C-Eintrag in den Boden gew&#228;hrleistet, auf die gew&#252;nschte zus&#228;tzliche SOC-Akkumulation und zum anderen am Fehlen geeigneter Versuchsans&#228;tze, um die Wirkung aller relevanten Faktoren gleichzeitig zu erfassen. Um diese Probleme zu l&#246;sen, wurde ein dreifaktorieller experimenteller Feldversuch angelegt: I.) "moderate Mutterbodenverd&#252;nnung" (verd&#252;nnt vs. unverd&#252;nnt), II.) "N-D&#252;ngeform" (mineralisch, d.h. Kalkammonsalpeter und Harnstoff vs. organisch, d.h. G&#228;rrest) und III.)  "Bodentypen" (Calcic Luvisol, Nudiargic Luvisol und Calcaric Regosol), die das typische Spektrum der Erosionszust&#228;nde in der h&#252;geligen Grundmor&#228;nenlandschaft Nordostdeutschlands abdecken. 
Diese Datenssammlung enth&#228;lt Wetterdaten, NDVI/RVI-Messungen, Bodentexturdaten, Boden- und Pflanzenanalysedaten sowie CO2-Fl&#252;sse, die mit einem neuartigen Roboterkammersystem im Zeitraum vom 23.07.2020 (nach der Manipulation) bis zum 29.06.2021 (Ernte) ermittelt wurden.
Diese Tabelle enth&#228;lt den Index aller Tabellen, die diese Datensammlung bilden.

Zugeh&#246;rige Datens&#228;tze sind unter Related Identifier gelistet.
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2024-04-11 Data imported to database
2024-04-19 Metadata xml for dataset created
2024-04 Dataset published in BonaRes Repository
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