<?xml version="1.0" encoding="utf-8"?>
<journal>
<title>Iranian Jornal of Watershed Management Science&amp;Engineering</title>
<title_fa>مجله علوم ومهندسی آبخیزداری ایران</title_fa>
<short_title>jwmseir</short_title>
<subject>Agriculture</subject>
<web_url>http://jwmsei.ir</web_url>
<journal_hbi_system_id>1</journal_hbi_system_id>
<journal_hbi_system_user>admin</journal_hbi_system_user>
<journal_id_issn>2008-9554</journal_id_issn>
<journal_id_issn_online>2008-9554</journal_id_issn_online>
<journal_id_pii>8</journal_id_pii>
<journal_id_doi>10.22034</journal_id_doi>
<journal_id_iranmedex></journal_id_iranmedex>
<journal_id_magiran></journal_id_magiran>
<journal_id_sid>14</journal_id_sid>
<journal_id_nlai>8888</journal_id_nlai>
<journal_id_science>13</journal_id_science>
<language>fa</language>
<pubdate>
	<type>jalali</type>
	<year>1404</year>
	<month>2</month>
	<day>1</day>
</pubdate>
<pubdate>
	<type>gregorian</type>
	<year>2025</year>
	<month>5</month>
	<day>1</day>
</pubdate>
<volume>19</volume>
<number>68</number>
<publish_type>online</publish_type>
<publish_edition>1</publish_edition>
<article_type>fulltext</article_type>
<articleset>
	<article>


	<language>fa</language>
	<article_id_doi></article_id_doi>
	<title_fa>بررسی تغییرات مکانی- زمانی ویژگی‌های کیفی آب مورد استفاده در بخش کشاورزی دشت ملایر</title_fa>
	<title>Spatial-Temporal Assessment of Groundwater Quality Characteristics for Agricultural Use in Malayer Plain</title>
	<subject_fa>تخصصي</subject_fa>
	<subject>Special</subject>
	<content_type_fa>پژوهشي</content_type_fa>
	<content_type>Research</content_type>
	<abstract_fa>&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;direction:rtl&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span bold=&quot;&quot; new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:-0.5pt&quot;&gt;&lt;span style=&quot;font-weight:bold&quot;&gt;&lt;span b=&quot;&quot; lang=&quot;AR-SA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;آب زیرزمینی از مهم&amp;shy;ترین منابع تأمین آب کشاورزی در مناطق خشک و نیمه&#8204;خشک است. &lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;استخراج بی&#8204;رویه آب از سفره&#8204;های آب زیرزمینی، منجر به تخریب کیفی و کمی آبخوان&#8204;ها و کاهش پتانسیل آن&#8204;ها برای تأمین آب می&#8204;شود&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;این پژوهش با هدف بررسی تغییرات مکانی و زمانی کیفیت آب زیرزمینی در دشت ملایر استان همدان طی دوره آماری پنج&#8204;ساله 1395 تا 1399 انجام شد. با توجه به نقش حیاتی آب زیرزمینی در کشاورزی مناطق خشک و نیمه&#8204;خشک و تهدیدهای ناشی از بهره&#8204;برداری بی&#8204;رویه، از روش&#8204;های درون&#8204;یابی زمین&#8204;آمار شامل کریجینگ (معمولی، عام و ساده) و&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;IDW&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;در محیط نرم&#8204;افزار&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;ArcGIS 10 &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;برای تهیه نقشه&#8204;های پهنه&#8204;بندی پارامترهای کیفی&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;EC&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;pH&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;HCO3&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;&amp;nbsp;CL&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;و&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt; SAR&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;در دو مقطع زمانی خرداد و شهریور استفاده شد. داده&#8204;های مورد نیاز از 31 حلقه چاه تأمین و دقت روش&#8204;ها با شاخص&#8204;های آماری مانند میانگین خطا و ریشه میانگین مربع خطا ارزیابی شد. نتایج نشان داد که دقت روش&#8204;ها بسته به پارامتر و زمان متفاوت است، به&#8204;گونه&#8204;ای که در ماه خرداد، روش کریجینگ معمولی برای اکثر پارامترها بهترین عملکرد را داشت، در حالی که در شهریور ترکیبی از کریجینگ و&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;IDW&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;بهینه بود. با استفاده از شاخص ویلکاکس، کیفیت آب برای کشاورزی در چهار کلاس ارزیابی و نقشه&#8204;های طبقه&#8204;بندی&#8204;شده با زبان برنامه&#8204;نویسی پایتون تولید شد. تحلیل تغییرات نشان داد که کیفیت آب در پارامترهایی چون&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;EC&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;، &lt;/span&gt;&lt;/span&gt;&amp;nbsp;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;HCO3&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;و&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt; CL&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;در دوره انتهایی نسبت به ابتدای دوره کاهش داشته و غلظت آن&#8204;ها افزایش یافته است، در حالی که تغییرات&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;pH&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;و&lt;/span&gt;&lt;/span&gt; &lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;SAR&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt; &lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;کم&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&amp;shy;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;تر بوده&#8204;اند. همچنین مساحت مناطقی با کیفیت &amp;quot;خوب&amp;quot; به&#8204;ترتیب در خرداد و شهریور &lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;span style=&quot;font-weight:normal&quot;&gt;به میزان 9/4 و 3/12 درصد&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt; کاهش یافته است. هیچ&#8204;یک از مناطق در کلاس &amp;quot;نامناسب&amp;quot; قرار نگرفتند، اما بخش&#8204;هایی از نواحی مرکزی و جنوب&#8204;شرقی در کلاس &amp;quot;متوسط&amp;quot; قرار گرفته و مستعد بحران هستند. نتایج بیانگر کارایی بالای روش&#8204;های درون&#8204;یابی در پایش و مدیریت منابع آب زیرزمینی بوده و استفاده مستمر از آن&#8204;ها برای حفظ پایداری منابع آب کشاورزی منطقه پیشنهاد می&#8204;شود&lt;/span&gt;&lt;/span&gt;&lt;span dir=&quot;LTR&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;span b=&quot;&quot; lang=&quot;FA&quot; lotus=&quot;&quot; style=&quot;font-family:&quot;&gt;&lt;span style=&quot;letter-spacing:0pt&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract_fa>
	<abstract>&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:9.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Abstract&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:9.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt; Abstract&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:9.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Introduction&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span dir=&quot;RTL&quot; lang=&quot;FA&quot; style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span style=&quot;font-family:&quot;B Nazanin&quot;&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Groundwater is a vital resource for agricultural water supply, particularly in arid and semi-arid regions. Overextraction of groundwater aquifers has led to both qualitative and quantitative degradation, reducing their potential for sustainable water supply. Monitoring spatial and temporal variations in agricultural water quality is essential for efficient utilization and aligning water quality parameters with agricultural usage. Geostatistics has emerged as a powerful tool across various disciplines, especially for interpolation and estimation tasks. Numerous methods are available for studying and mapping groundwater quality variations, with their accuracy depending on regional conditions and data availability. Previous research highlights the reliability of interpolation methods in generating groundwater quality maps. Thus, creating groundwater quality maps using local data and appropriate spatial analysis methods is vital for water resource management. This study evaluates geostatistical methods to analyze spatial and temporal variations in groundwater quality parameters for agricultural purposes in Malayer Plain, Hamadan Province.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Methodology&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&amp;nbsp;The study area encompasses the main aquifer of Malayer Plain in Hamadan Province, with an area of 518.63 km&amp;sup2;. Data from 31 wells, provided by the Hamadan Regional Water Company, were used to analyze groundwater quality parameters. These parameters included EC, pH, HCO₃, CL, and SAR, measured during June and September over a five-year period (2016&amp;ndash;2020). Zoning maps were created using Inverse Distance Weighting (IDW) and Kriging (Ordinary, Universal, and Simple) methods with exponential, Gaussian, and spherical variograms in ArcGIS 10. The accuracy of the zoning methods was evaluated using statistical metrics such as Mean Error (ME), Root Mean Square Error (RMSE), and Root Mean Square Standardized Error (RMSSE). The best interpolation method for each parameter was selected based on these metrics. Temporal variations in groundwater quality parameters were assessed by generating algebraic maps using the Raster Calculator tool, dividing the parameter values for June and September 2020 by those from 2016. Continuous classified maps were created using the Wilcox agricultural water quality index implemented via Python scripting in ArcGIS 10.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Results and Discussion&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;In June, the most suitable interpolation methods for each parameter were Ordinary Kriging, Universal Kriging, IDW, and Ordinary Kriging, respectively. In September, the preferred methods for EC, pH, HCO₃, CL, and SAR were Ordinary Kriging, Universal Kriging, IDW, Ordinary Kriging, and IDW, respectively. Groundwater quality was classified into four standard classes&amp;mdash;excellent, good, medium, and poor&amp;mdash;based on EC and SAR. Maps of agricultural water quality standards were developed for June and September. The SAR parameter exhibited a stable trend in June but showed significant fluctuations in September, particularly in 2017. For EC, despite an increasing trend in both months, values were consistently lower in June compared to September. According to the Wilcox index, areas classified as &amp;quot;good&amp;quot; quality decreased by 4.9% from 2016 to 2020 in June and by 12.3% in September.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;b&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;Conclusion&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;b&gt;&lt;span style=&quot;font-size:9.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;/span&gt;&lt;/span&gt;&lt;/b&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&amp;nbsp;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;This study utilized GIS tools to determine the quality standards for agricultural water and analyze spatial-temporal variations in groundwater quality parameters in the saturated aquifer of Malayer Plain. Python scripting was employed to produce classified raster maps based on the Wilcox index. The results indicated that the geostatistical methods used were sufficiently accurate for the study area. Kriging and IDW provided the best interpolation accuracy. The analysis covered five years of data for June and September, focusing on EC, pH, HCO₃, CL, and SAR. The results showed declining groundwater quality, with increased concentrations of CL, HCO₃, and EC over time, while slight reductions were observed for pH and SAR. None of the areas were classified as &amp;quot;poor&amp;quot; according to the Wilcox index, but central and southeastern parts of the aquifer fell into the &amp;quot;medium&amp;quot; class, indicating vulnerability to critical conditions. Given the importance of groundwater quality for agriculture, the environment, and the economy, the continued application of interpolation methods can serve as a fast and effective approach for groundwater quality monitoring in Malayer Plain.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&lt;span style=&quot;font-size:11pt&quot;&gt;&lt;span style=&quot;unicode-bidi:embed&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;&lt;span new=&quot;&quot; roman=&quot;&quot; style=&quot;font-family:&quot; times=&quot;&quot;&gt;&lt;span style=&quot;font-size:10.0pt&quot;&gt;&lt;span style=&quot;line-height:107%&quot;&gt;.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;br&gt;
&amp;nbsp;</abstract>
	<keyword_fa>ملایر, آب‌زیرزمینی, خشک‌سالی, زمین‌آمار, ویلکاکس</keyword_fa>
	<keyword>Malayer, Groundwater, Drought, Land statistics, Wilcox</keyword>
	<start_page>78</start_page>
	<end_page>92</end_page>
	<web_url>http://jwmsei.ir/browse.php?a_code=A-10-1654-1&amp;slc_lang=fa&amp;sid=1</web_url>


<author_list>
	<author>
	<first_name>Samira</first_name>
	<middle_name></middle_name>
	<last_name>Alsadat Hedayati</last_name>
	<suffix></suffix>
	<first_name_fa>سمیراالسادات</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>هدایتی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>s.hedayti@basu.ac.ir</email>
	<code>100319475328460018946</code>
	<orcid>0009-0008-7945-3948</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Water Science and Engineering, Boali-Sina University, Hamadan, Iran.</affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>Omid</first_name>
	<middle_name></middle_name>
	<last_name>Bahmani</last_name>
	<suffix></suffix>
	<first_name_fa>امید</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>بهمنی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>omid.bahmani@basu.ac.ir</email>
	<code>100319475328460018947</code>
	<orcid>100319475328460018947</orcid>
	<coreauthor>Yes
</coreauthor>
	<affiliation>Department of Water Science and Engineering, Boali-Sina University, Hamadan, Iran.</affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>Peyman</first_name>
	<middle_name></middle_name>
	<last_name>Tahmasebi</last_name>
	<suffix></suffix>
	<first_name_fa>پیمان</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>طهماسبی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>p.tahmasebi@agr.basu.ac.ir</email>
	<code>100319475328460018948</code>
	<orcid>0009-0003-1316-2260</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Water Science and Engineering, Boali-Sina University, Hamadan, Iran.</affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>Fatemeh</first_name>
	<middle_name></middle_name>
	<last_name>Dalvand</last_name>
	<suffix></suffix>
	<first_name_fa>فاطمه</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>دالوند</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>fatemedalvand7499@gmail.com</email>
	<code>100319475328460018949</code>
	<orcid>0009-0008-7347-975X</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Water Science and Engineering, Boali-Sina University, Hamadan, Iran.</affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


	<author>
	<first_name>Seyed Abolfazl</first_name>
	<middle_name></middle_name>
	<last_name>Hosseini</last_name>
	<suffix></suffix>
	<first_name_fa>سید ابولفضل</first_name_fa>
	<middle_name_fa></middle_name_fa>
	<last_name_fa>حسینی</last_name_fa>
	<suffix_fa></suffix_fa>
	<email>nemayeh22@gmail.com</email>
	<code>100319475328460018950</code>
	<orcid>0009-0008-0082-7768</orcid>
	<coreauthor>No</coreauthor>
	<affiliation>Department of Water Science and Engineering, Boali-Sina University, Hamadan, Iran.</affiliation>
	<affiliation_fa></affiliation_fa>
	 </author>


</author_list>


	</article>
</articleset>
</journal>
