Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition

Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angul...
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Autor*in:	Rezapour, Salar [verfasserIn] Kalashypour, E. Asadzadeh, F.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Salt-affected soil Soil quality Soil improvement Irrigation and cultivation Semi-arid condition

Anmerkung:	© University of Tehran 2017

Übergeordnetes Werk:	Enthalten in: International journal of environmental research - [Cham] : Springer International Publishing, 2007, 11(2017), 3 vom: 12. Juni, Seite 301-313
Übergeordnetes Werk:	volume:11 ; year:2017 ; number:3 ; day:12 ; month:06 ; pages:301-313

Links:	Volltext

DOI / URN:	10.1007/s41742-017-0028-0

Katalog-ID:	SPR038290766

Internformat


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520			\|a Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region.
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publishDate	2017
allfields	10.1007/s41742-017-0028-0 doi (DE-627)SPR038290766 (SPR)s41742-017-0028-0-e DE-627 ger DE-627 rakwb eng Rezapour, Salar verfasserin aut Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © University of Tehran 2017 Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213 Kalashypour, E. aut Asadzadeh, F. aut Enthalten in International journal of environmental research [Cham] : Springer International Publishing, 2007 11(2017), 3 vom: 12. Juni, Seite 301-313 (DE-627)552252506 (DE-600)2399844-1 2008-2304 nnns volume:11 year:2017 number:3 day:12 month:06 pages:301-313 https://dx.doi.org/10.1007/s41742-017-0028-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_266 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_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_2118 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_2472 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 11 2017 3 12 06 301-313
spelling	10.1007/s41742-017-0028-0 doi (DE-627)SPR038290766 (SPR)s41742-017-0028-0-e DE-627 ger DE-627 rakwb eng Rezapour, Salar verfasserin aut Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © University of Tehran 2017 Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213 Kalashypour, E. aut Asadzadeh, F. aut Enthalten in International journal of environmental research [Cham] : Springer International Publishing, 2007 11(2017), 3 vom: 12. Juni, Seite 301-313 (DE-627)552252506 (DE-600)2399844-1 2008-2304 nnns volume:11 year:2017 number:3 day:12 month:06 pages:301-313 https://dx.doi.org/10.1007/s41742-017-0028-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_266 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_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_2118 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_2472 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 11 2017 3 12 06 301-313
allfields_unstemmed	10.1007/s41742-017-0028-0 doi (DE-627)SPR038290766 (SPR)s41742-017-0028-0-e DE-627 ger DE-627 rakwb eng Rezapour, Salar verfasserin aut Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © University of Tehran 2017 Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213 Kalashypour, E. aut Asadzadeh, F. aut Enthalten in International journal of environmental research [Cham] : Springer International Publishing, 2007 11(2017), 3 vom: 12. Juni, Seite 301-313 (DE-627)552252506 (DE-600)2399844-1 2008-2304 nnns volume:11 year:2017 number:3 day:12 month:06 pages:301-313 https://dx.doi.org/10.1007/s41742-017-0028-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_266 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_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_2118 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_2472 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 11 2017 3 12 06 301-313
allfieldsGer	10.1007/s41742-017-0028-0 doi (DE-627)SPR038290766 (SPR)s41742-017-0028-0-e DE-627 ger DE-627 rakwb eng Rezapour, Salar verfasserin aut Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © University of Tehran 2017 Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213 Kalashypour, E. aut Asadzadeh, F. aut Enthalten in International journal of environmental research [Cham] : Springer International Publishing, 2007 11(2017), 3 vom: 12. Juni, Seite 301-313 (DE-627)552252506 (DE-600)2399844-1 2008-2304 nnns volume:11 year:2017 number:3 day:12 month:06 pages:301-313 https://dx.doi.org/10.1007/s41742-017-0028-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_266 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_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_2118 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_2472 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 11 2017 3 12 06 301-313
allfieldsSound	10.1007/s41742-017-0028-0 doi (DE-627)SPR038290766 (SPR)s41742-017-0028-0-e DE-627 ger DE-627 rakwb eng Rezapour, Salar verfasserin aut Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © University of Tehran 2017 Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213 Kalashypour, E. aut Asadzadeh, F. aut Enthalten in International journal of environmental research [Cham] : Springer International Publishing, 2007 11(2017), 3 vom: 12. Juni, Seite 301-313 (DE-627)552252506 (DE-600)2399844-1 2008-2304 nnns volume:11 year:2017 number:3 day:12 month:06 pages:301-313 https://dx.doi.org/10.1007/s41742-017-0028-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_266 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_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_2118 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_2472 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 11 2017 3 12 06 301-313
language	English
source	Enthalten in International journal of environmental research 11(2017), 3 vom: 12. Juni, Seite 301-313 volume:11 year:2017 number:3 day:12 month:06 pages:301-313
sourceStr	Enthalten in International journal of environmental research 11(2017), 3 vom: 12. Juni, Seite 301-313 volume:11 year:2017 number:3 day:12 month:06 pages:301-313
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Salt-affected soil Soil quality Soil improvement Irrigation and cultivation Semi-arid condition
isfreeaccess_bool	false
container_title	International journal of environmental research
authorswithroles_txt_mv	Rezapour, Salar @@aut@@ Kalashypour, E. @@aut@@ Asadzadeh, F. @@aut@@
publishDateDaySort_date	2017-06-12T00:00:00Z
hierarchy_top_id	552252506
id	SPR038290766
language_de	englisch
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author	Rezapour, Salar
spellingShingle	Rezapour, Salar misc Salt-affected soil misc Soil quality misc Soil improvement misc Irrigation and cultivation misc Semi-arid condition Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition
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topic_title	Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition Salt-affected soil (dpeaa)DE-He213 Soil quality (dpeaa)DE-He213 Soil improvement (dpeaa)DE-He213 Irrigation and cultivation (dpeaa)DE-He213 Semi-arid condition (dpeaa)DE-He213
topic	misc Salt-affected soil misc Soil quality misc Soil improvement misc Irrigation and cultivation misc Semi-arid condition
topic_unstemmed	misc Salt-affected soil misc Soil quality misc Soil improvement misc Irrigation and cultivation misc Semi-arid condition
topic_browse	misc Salt-affected soil misc Soil quality misc Soil improvement misc Irrigation and cultivation misc Semi-arid condition
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title	Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition
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title_full	Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition
author_sort	Rezapour, Salar
journal	International journal of environmental research
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author_browse	Rezapour, Salar Kalashypour, E. Asadzadeh, F.
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doi_str_mv	10.1007/s41742-017-0028-0
title_sort	assessment of the quality of salt-affected soils after irrigation and cultivation in semi-arid condition
title_auth	Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition
abstract	Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. © University of Tehran 2017
abstractGer	Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. © University of Tehran 2017
abstract_unstemmed	Abstract This study investigates morphological, physicochemical properties and clay mineralogy of four soil types belonging to salt-affected soils after converting into cropland. The data showed that strong platy to the medium prismatic structure of salt-affected soils was replaced by the fine angular blocky structure in cropland mainly as a result of the improvement in organic matter caused by agricultural practices and wetting–drying cycle accelerated by irrigation. After cultivation, two decreasing and increasing trends were observed in clay content (a drop of 17–51%) and sand (a rise of 8–96%), respectively. There was a remarked depletion in the values of soil pH (0.17–0.78 unit), calcium carbonate equivalent (8–30%), EC (50–82%), SAR (60–85%), exchangeable Na (53–77%), and ESP (46–65%) with cultivation, whereas the amounts of organic carbon (13–130%), total N (27–157%), and exchangeable Ca and Mg (20–60%) were increased after cultivation, indicating the improvement in the soil chemical indicators when converting salt-affected soils to cropland. Soil erodibility factor (K-factor), evaluated based on some physicochemical properties, revealed that 75% of the soils had a decreasing pattern in the K-factor and 25% had an increasing pattern after cultivation. The significant change was not observed in the XRD patterns of the clay fraction by cultivation. Overall, it can conclude that continuous tillage and irrigation-cropping can be a useful method for quality restoration of salt-affected soils in the region. © University of Tehran 2017
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title_short	Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition
url	https://dx.doi.org/10.1007/s41742-017-0028-0
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Assessment of the Quality of Salt-Affected Soils After Irrigation and Cultivation in Semi-arid Condition

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