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<Article>
<Journal>
				<PublisherName>Isfahan University of Technology</PublisherName>
				<JournalTitle>Dryland Soil Research (DLSR)</JournalTitle>
				<Issn>3115-9486</Issn>
				<Volume>2</Volume>
				<Issue>1</Issue>
				<PubDate PubStatus="epublish">
					<Year>2025</Year>
					<Month>03</Month>
					<Day>01</Day>
				</PubDate>
			</Journal>
<ArticleTitle>Prediction of soil potassium forms using physicochemical properties and exchangeable potassium: II. Influence of soil properties on potassium distribution</ArticleTitle>
<VernacularTitle></VernacularTitle>
			<FirstPage>81</FirstPage>
			<LastPage>88</LastPage>
			<ELocationID EIdType="pii">3735</ELocationID>
			
<ELocationID EIdType="doi">10.47176/dlsr.02.01.1043</ELocationID>
			
			<Language>EN</Language>
<AuthorList>
<Author>
					<FirstName>Manoochehr</FirstName>
					<LastName>Gholipoor</LastName>
<Affiliation>Deparment of Soil Science, College of Agriculture, Shahrood University of Technology, 3619995161, Shahrood, Iran</Affiliation>
<Identifier Source="ORCID">0000-0001-9229-4744</Identifier>

</Author>
</AuthorList>
				<PublicationType>Journal Article</PublicationType>
			<History>
				<PubDate PubStatus="received">
					<Year>2025</Year>
					<Month>07</Month>
					<Day>30</Day>
				</PubDate>
			</History>
		<Abstract>A quantitative understanding of the factors regulating potassium (K) distribution in soils is essential for optimizing nutrient management in agricultural systems, as K availability directly influences crop productivity and soil health. To systematically evaluate the drivers of K dynamics, a suite of artificial neural networks, coupled with Deep Learning Important FeaTures (DeepLIFT) attribution analysis, was employed to quantitatively assess the relative influence of key soil properties, including clay, silt, and sand content, pH, organic carbon (OC), cation exchange capacity (CEC), and electrical conductivity (EC), on four distinct K pools: water-soluble K, non-exchangeable K, fixed K, and total K. Additionally, the study investigated the association of soil initial water-soluble K and fertilizer K application rate with the fixation of K fertilizer to elucidate the relationship between them. Key findings revealed divergent drivers across K fractions, highlighting the complexity of K dynamics in soils. CEC emerged as the dominant factor influencing water-soluble K variability (+22.43%), underscoring its role in regulating K mobility. Clay content exhibited contrasting effects, positively influencing non-exchangeable K (+13.42%), total K (+20.59%), and fixed K (+13.81%), while negatively impacting water-soluble K (-14.38%). EC was the primary determinant of non-exchangeable K (+34.27%), suggesting salinity’s role in K retention. In contrast, pH showed a strong association with fixed K (+26.58%), reflecting its influence on interlayer trapping within 2:1 clay minerals. To bridge predictive modeling and practical applications, a genetic algorithm was integrated into an open-source, user-friendly Excel-based tool. This tool enables farmers and agronomists to optimize soil conditions for maximizing the sum of water-soluble and exchangeable K (plant-available K), thereby supporting precision nutrient management. By elucidating soil-specific K dynamics and providing actionable insights, this research advances sustainable K stewardship. The tool is accessible for download at: https://drive.shahroodut.ac.ir/index.php/s/fayE0zUH16TQe2M</Abstract>
		<ObjectList>
			<Object Type="keyword">
			<Param Name="value">Potassium fractions</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Soil physicochemical properties</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Artificial Neural Network</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">Genetic algorithm optimization</Param>
			</Object>
			<Object Type="keyword">
			<Param Name="value">DeepLIFT feature attribution</Param>
			</Object>
		</ObjectList>
<ArchiveCopySource DocType="pdf">https://dlsr.iut.ac.ir/article_3735_dc0c398086fee58f9d64e1e47aa4e586.pdf</ArchiveCopySource>
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