The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system)
Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lo...
Ausführliche Beschreibung
Autor*in: |
Gorokhova, I. N. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2017 |
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Schlagwörter: |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2017 |
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Übergeordnetes Werk: |
Enthalten in: Arid ecosystems - Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011, 7(2017), 3 vom: Juli, Seite 161-170 |
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Übergeordnetes Werk: |
volume:7 ; year:2017 ; number:3 ; month:07 ; pages:161-170 |
Links: |
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DOI / URN: |
10.1134/S2079096117030052 |
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Katalog-ID: |
SPR031372554 |
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520 | |a Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. | ||
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10.1134/S2079096117030052 doi (DE-627)SPR031372554 (SPR)S2079096117030052-e DE-627 ger DE-627 rakwb eng Gorokhova, I. N. verfasserin aut The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 Pankova, E. I. aut Enthalten in Arid ecosystems Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011 7(2017), 3 vom: Juli, Seite 161-170 (DE-627)656334622 (DE-600)2603446-3 2079-0988 nnns volume:7 year:2017 number:3 month:07 pages:161-170 https://dx.doi.org/10.1134/S2079096117030052 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_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_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 7 2017 3 07 161-170 |
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10.1134/S2079096117030052 doi (DE-627)SPR031372554 (SPR)S2079096117030052-e DE-627 ger DE-627 rakwb eng Gorokhova, I. N. verfasserin aut The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 Pankova, E. I. aut Enthalten in Arid ecosystems Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011 7(2017), 3 vom: Juli, Seite 161-170 (DE-627)656334622 (DE-600)2603446-3 2079-0988 nnns volume:7 year:2017 number:3 month:07 pages:161-170 https://dx.doi.org/10.1134/S2079096117030052 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_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_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 7 2017 3 07 161-170 |
allfields_unstemmed |
10.1134/S2079096117030052 doi (DE-627)SPR031372554 (SPR)S2079096117030052-e DE-627 ger DE-627 rakwb eng Gorokhova, I. N. verfasserin aut The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 Pankova, E. I. aut Enthalten in Arid ecosystems Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011 7(2017), 3 vom: Juli, Seite 161-170 (DE-627)656334622 (DE-600)2603446-3 2079-0988 nnns volume:7 year:2017 number:3 month:07 pages:161-170 https://dx.doi.org/10.1134/S2079096117030052 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_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_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 7 2017 3 07 161-170 |
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10.1134/S2079096117030052 doi (DE-627)SPR031372554 (SPR)S2079096117030052-e DE-627 ger DE-627 rakwb eng Gorokhova, I. N. verfasserin aut The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 Pankova, E. I. aut Enthalten in Arid ecosystems Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011 7(2017), 3 vom: Juli, Seite 161-170 (DE-627)656334622 (DE-600)2603446-3 2079-0988 nnns volume:7 year:2017 number:3 month:07 pages:161-170 https://dx.doi.org/10.1134/S2079096117030052 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_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_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 7 2017 3 07 161-170 |
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10.1134/S2079096117030052 doi (DE-627)SPR031372554 (SPR)S2079096117030052-e DE-627 ger DE-627 rakwb eng Gorokhova, I. N. verfasserin aut The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 Pankova, E. I. aut Enthalten in Arid ecosystems Dordrecht [u.a.] : Springer Science + Business Media B.V, 2011 7(2017), 3 vom: Juli, Seite 161-170 (DE-627)656334622 (DE-600)2603446-3 2079-0988 nnns volume:7 year:2017 number:3 month:07 pages:161-170 https://dx.doi.org/10.1134/S2079096117030052 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_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_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 7 2017 3 07 161-170 |
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Gorokhova, I. N. |
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Gorokhova, I. N. misc patchiness of irrigation soils misc nature of soil patchiness The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) |
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The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) patchiness of irrigation soils (dpeaa)DE-He213 nature of soil patchiness (dpeaa)DE-He213 |
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misc patchiness of irrigation soils misc nature of soil patchiness |
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The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) |
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The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) |
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nature of the patchiness of irrigated soils in the dry steppe zone (on example of the svetloyarskaya irrigation system) |
title_auth |
The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) |
abstract |
Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. © Pleiades Publishing, Ltd. 2017 |
abstractGer |
Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. © Pleiades Publishing, Ltd. 2017 |
abstract_unstemmed |
Abstract Various variants of the patchiness of irrigated soils, which are reflected on remote sensing materials and associated with the results of field research, have been analyzed on the example of the Svetloyarskaya irrigation system. The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others. © Pleiades Publishing, Ltd. 2017 |
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title_short |
The nature of the patchiness of irrigated soils in the dry steppe zone (on example of the Svetloyarskaya irrigation system) |
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https://dx.doi.org/10.1134/S2079096117030052 |
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The system is located on the right-bank part of the Caspian lowland within the solonetz complexes of the dry steppe. It is revealed that the reasons for the formation of the patchiness of irrigated fields fixed on remote materials are not unambiguous. During studies at the Svetloyarskaya irrigation system, it was found that the patchiness depends on the depth of the groundwater table (GWT) and the state of the field (bare soil, cropland, and layland) and can be caused by soil properties, such as primary and secondary salinization, alkalization, the carbonate content, and others.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">patchiness of irrigation soils</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">nature of soil patchiness</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Pankova, E. 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