Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq

Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals con...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Saleh, Amal Muhammad [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Schlagwörter:	Spatial variability Semivariogram Cross-semivariogram Kriging Co kriging

Übergeordnetes Werk:	Enthalten in: Journal of the Indian Society of Remote Sensing - Neu Delhi : Springer India, 2008, 46(2018), 9 vom: 16. Juli, Seite 1481-1495
Übergeordnetes Werk:	volume:46 ; year:2018 ; number:9 ; day:16 ; month:07 ; pages:1481-1495

Links:	Volltext

DOI / URN:	10.1007/s12524-018-0795-x

Katalog-ID:	SPR026025027

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520			\|a Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study.
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matchkey_str	article:09743006:2018----::ptavraiiyapnosmsipoeteijdaa_
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publishDate	2018
allfields	10.1007/s12524-018-0795-x doi (DE-627)SPR026025027 (SPR)s12524-018-0795-x-e DE-627 ger DE-627 rakwb eng 550 ASE Saleh, Amal Muhammad verfasserin aut Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study. Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213 Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 46(2018), 9 vom: 16. Juli, Seite 1481-1495 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495 https://dx.doi.org/10.1007/s12524-018-0795-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 46 2018 9 16 07 1481-1495
spelling	10.1007/s12524-018-0795-x doi (DE-627)SPR026025027 (SPR)s12524-018-0795-x-e DE-627 ger DE-627 rakwb eng 550 ASE Saleh, Amal Muhammad verfasserin aut Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study. Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213 Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 46(2018), 9 vom: 16. Juli, Seite 1481-1495 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495 https://dx.doi.org/10.1007/s12524-018-0795-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 46 2018 9 16 07 1481-1495
allfields_unstemmed	10.1007/s12524-018-0795-x doi (DE-627)SPR026025027 (SPR)s12524-018-0795-x-e DE-627 ger DE-627 rakwb eng 550 ASE Saleh, Amal Muhammad verfasserin aut Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study. Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213 Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 46(2018), 9 vom: 16. Juli, Seite 1481-1495 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495 https://dx.doi.org/10.1007/s12524-018-0795-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 46 2018 9 16 07 1481-1495
allfieldsGer	10.1007/s12524-018-0795-x doi (DE-627)SPR026025027 (SPR)s12524-018-0795-x-e DE-627 ger DE-627 rakwb eng 550 ASE Saleh, Amal Muhammad verfasserin aut Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study. Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213 Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 46(2018), 9 vom: 16. Juli, Seite 1481-1495 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495 https://dx.doi.org/10.1007/s12524-018-0795-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 46 2018 9 16 07 1481-1495
allfieldsSound	10.1007/s12524-018-0795-x doi (DE-627)SPR026025027 (SPR)s12524-018-0795-x-e DE-627 ger DE-627 rakwb eng 550 ASE Saleh, Amal Muhammad verfasserin aut Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study. Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213 Enthalten in Journal of the Indian Society of Remote Sensing Neu Delhi : Springer India, 2008 46(2018), 9 vom: 16. Juli, Seite 1481-1495 (DE-627)573088853 (DE-600)2439566-3 0974-3006 nnns volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495 https://dx.doi.org/10.1007/s12524-018-0795-x kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 46 2018 9 16 07 1481-1495
language	English
source	Enthalten in Journal of the Indian Society of Remote Sensing 46(2018), 9 vom: 16. Juli, Seite 1481-1495 volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495
sourceStr	Enthalten in Journal of the Indian Society of Remote Sensing 46(2018), 9 vom: 16. Juli, Seite 1481-1495 volume:46 year:2018 number:9 day:16 month:07 pages:1481-1495
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Spatial variability Semivariogram Cross-semivariogram Kriging Co kriging
dewey-raw	550
isfreeaccess_bool	true
container_title	Journal of the Indian Society of Remote Sensing
authorswithroles_txt_mv	Saleh, Amal Muhammad @@aut@@
publishDateDaySort_date	2018-07-16T00:00:00Z
hierarchy_top_id	573088853
dewey-sort	3550
id	SPR026025027
language_de	englisch
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author	Saleh, Amal Muhammad
spellingShingle	Saleh, Amal Muhammad ddc 550 misc Spatial variability misc Semivariogram misc Cross-semivariogram misc Kriging misc Co kriging Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq
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topic_title	550 ASE Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq Spatial variability (dpeaa)DE-He213 Semivariogram (dpeaa)DE-He213 Cross-semivariogram (dpeaa)DE-He213 Kriging (dpeaa)DE-He213 Co kriging (dpeaa)DE-He213
topic	ddc 550 misc Spatial variability misc Semivariogram misc Cross-semivariogram misc Kriging misc Co kriging
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title	Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq
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title_full	Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq
author_sort	Saleh, Amal Muhammad
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title_sort	spatial variability mapping of some soil properties in jadwal al_amir project/babylon/iraq
title_auth	Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq
abstract	Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study.
abstractGer	Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study.
abstract_unstemmed	Abstract This study was carried out to identify and compare spatial variation of some soil physical and chemical properties in the Jadwal Al_Amir Project/Babylon/Iraq. Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. These results indicated that cokriging improved predictions for clay content with soil properties studied and considered to be an accurate and adequate procedure for spatial interpolation and evaluation of soil properties considered in this study.
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container_issue	9
title_short	Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq
url	https://dx.doi.org/10.1007/s12524-018-0795-x
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doi_str	10.1007/s12524-018-0795-x
up_date	2024-07-03T18:25:30.737Z
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Soil properties including soil texture fractions (sand, silt, clay), electrolytic conductivity (ECe), calcium carbonate minerals content ($ CaCO_{3} $), and organic matter content (O.M.) were measured by collecting soil samples from (0–30 cm) soil depths at 150 sampling sites. Soil properties were analyzed using both classical and geostatistical methods that included descriptive statistics, semivariograms, cross-semivariograms spatial kriged and co-kriged prediction maps and interpolation. Results indicated that moderate to strong spatial variability existed across the study area for soil properties considered in this study. Strong spatial dependency of soil properties was related to structural intrinsic factors such as parent material and mineralogy. Furthermore, cross-semivariograms exhibited a strong spatial interdependency between clay content with sqrtECe, $ CaCO_{3} $ minerals content, and log O.M. content. 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Spatial Variability Mapping of Some Soil Properties in Jadwal Al_Amir Project/Babylon/Iraq

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