HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN

The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the k...
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Autor*in:	osé Geraldo de Melo [verfasserIn] Adriana Barroca de Medeiros [verfasserIn] Mickaelon Belchior Vasconcelos [verfasserIn] Vera Lúcia Lopes de Castro [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch ; Portugiesisch

Erschienen:	2007

Schlagwörter:	Bacia Potiguar Formação Jandaíra carste irrigação Potiguar Basin Jandaíra Formation karst irrigation

Übergeordnetes Werk:	In: Revista Águas Subterrâneas - Associação Brasileira de Águas Subterrâneas, 2017, 21(2007), 1
Übergeordnetes Werk:	volume:21 ; year:2007 ; number:1

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.14295/ras.v21i1.16161

Katalog-ID:	DOAJ010610715

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spelling	10.14295/ras.v21i1.16161 doi (DE-627)DOAJ010610715 (DE-599)DOAJ0de2d2ec977b4be19d10c6ca7a2d554e DE-627 ger DE-627 rakwb eng por TC401-506 GB3-5030 osé Geraldo de Melo verfasserin aut HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. In this case the water is Ca-HCO3 type water, with lowsalinity and in most of the cases it is good to human use and irrigation (classes C2S1T1 e C2S1T2 to irrigation); To theSouthern part of Baraúna, where the karsts are less expressive, the groundwater salinity is high, Ca-Mg-Cl type water andthe quality suffers a certain restriction to human use and irrigation (Class C3S1T3). Bacia Potiguar Formação Jandaíra carste irrigação Potiguar Basin Jandaíra Formation karst irrigation River, lake, and water-supply engineering (General) Physical geography Adriana Barroca de Medeiros verfasserin aut Mickaelon Belchior Vasconcelos verfasserin aut Vera Lúcia Lopes de Castro verfasserin aut In Revista Águas Subterrâneas Associação Brasileira de Águas Subterrâneas, 2017 21(2007), 1 (DE-627)512661626 (DE-600)2236523-0 21799784 nnns volume:21 year:2007 number:1 https://doi.org/10.14295/ras.v21i1.16161 kostenfrei https://doaj.org/article/0de2d2ec977b4be19d10c6ca7a2d554e kostenfrei https://aguassubterraneas.abas.org/asubterraneas/article/view/16161 kostenfrei https://doaj.org/toc/0101-7004 Journal toc kostenfrei https://doaj.org/toc/2179-9784 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2007 1
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allfieldsSound	10.14295/ras.v21i1.16161 doi (DE-627)DOAJ010610715 (DE-599)DOAJ0de2d2ec977b4be19d10c6ca7a2d554e DE-627 ger DE-627 rakwb eng por TC401-506 GB3-5030 osé Geraldo de Melo verfasserin aut HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN 2007 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. In this case the water is Ca-HCO3 type water, with lowsalinity and in most of the cases it is good to human use and irrigation (classes C2S1T1 e C2S1T2 to irrigation); To theSouthern part of Baraúna, where the karsts are less expressive, the groundwater salinity is high, Ca-Mg-Cl type water andthe quality suffers a certain restriction to human use and irrigation (Class C3S1T3). Bacia Potiguar Formação Jandaíra carste irrigação Potiguar Basin Jandaíra Formation karst irrigation River, lake, and water-supply engineering (General) Physical geography Adriana Barroca de Medeiros verfasserin aut Mickaelon Belchior Vasconcelos verfasserin aut Vera Lúcia Lopes de Castro verfasserin aut In Revista Águas Subterrâneas Associação Brasileira de Águas Subterrâneas, 2017 21(2007), 1 (DE-627)512661626 (DE-600)2236523-0 21799784 nnns volume:21 year:2007 number:1 https://doi.org/10.14295/ras.v21i1.16161 kostenfrei https://doaj.org/article/0de2d2ec977b4be19d10c6ca7a2d554e kostenfrei https://aguassubterraneas.abas.org/asubterraneas/article/view/16161 kostenfrei https://doaj.org/toc/0101-7004 Journal toc kostenfrei https://doaj.org/toc/2179-9784 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 21 2007 1
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author	osé Geraldo de Melo
spellingShingle	osé Geraldo de Melo misc TC401-506 misc GB3-5030 misc Bacia Potiguar misc Formação Jandaíra misc carste misc irrigação misc Potiguar Basin misc Jandaíra Formation misc karst misc irrigation misc River, lake, and water-supply engineering (General) misc Physical geography HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN
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topic_title	TC401-506 GB3-5030 HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN Bacia Potiguar Formação Jandaíra carste irrigação Potiguar Basin Jandaíra Formation karst irrigation
topic	misc TC401-506 misc GB3-5030 misc Bacia Potiguar misc Formação Jandaíra misc carste misc irrigação misc Potiguar Basin misc Jandaíra Formation misc karst misc irrigation misc River, lake, and water-supply engineering (General) misc Physical geography
topic_unstemmed	misc TC401-506 misc GB3-5030 misc Bacia Potiguar misc Formação Jandaíra misc carste misc irrigação misc Potiguar Basin misc Jandaíra Formation misc karst misc irrigation misc River, lake, and water-supply engineering (General) misc Physical geography
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title_sort	hydrogeochemical aspects and water classes of the karst jandaíra aquifer for irrigation, baraúna, rn
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title_auth	HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN
abstract	The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. In this case the water is Ca-HCO3 type water, with lowsalinity and in most of the cases it is good to human use and irrigation (classes C2S1T1 e C2S1T2 to irrigation); To theSouthern part of Baraúna, where the karsts are less expressive, the groundwater salinity is high, Ca-Mg-Cl type water andthe quality suffers a certain restriction to human use and irrigation (Class C3S1T3).
abstractGer	The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. In this case the water is Ca-HCO3 type water, with lowsalinity and in most of the cases it is good to human use and irrigation (classes C2S1T1 e C2S1T2 to irrigation); To theSouthern part of Baraúna, where the karsts are less expressive, the groundwater salinity is high, Ca-Mg-Cl type water andthe quality suffers a certain restriction to human use and irrigation (Class C3S1T3).
abstract_unstemmed	The Baraúna region is situated on the West part of the Potiguar Basin, in the semi-arid domain of theRN State. Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. In this case the water is Ca-HCO3 type water, with lowsalinity and in most of the cases it is good to human use and irrigation (classes C2S1T1 e C2S1T2 to irrigation); To theSouthern part of Baraúna, where the karsts are less expressive, the groundwater salinity is high, Ca-Mg-Cl type water andthe quality suffers a certain restriction to human use and irrigation (Class C3S1T3).
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title_short	HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN
url	https://doi.org/10.14295/ras.v21i1.16161 https://doaj.org/article/0de2d2ec977b4be19d10c6ca7a2d554e https://aguassubterraneas.abas.org/asubterraneas/article/view/16161 https://doaj.org/toc/0101-7004 https://doaj.org/toc/2179-9784
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Its geology comprehends mainly carbonate rocks (calcareous and dolomites) of the Jandaíra Formation whose ageis attributed to the Superior Cretaceous. This geological unit constitutes the karst Jandaíra Aquifer, which is the main watersupply source to human use and irrigation. The Jandaíra Aquifer develops different levels of karst in the different sectors ofthe area, affecting the groundwater potentialities and its quality. In this article aspects in relation to the groundwater use andsalinization are presented, highlighting the groundwater use to irrigation. It was developed using data obtained fromgeophysical studies, wells cadastre, topographic studies and the interpretation of the hydrochemistry data. In the Northernand Western sectors of Baraúna the karsts are more expressive. 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HYDROGEOCHEMICAL ASPECTS AND WATER CLASSES OF THE KARST JANDAÍRA AQUIFER FOR IRRIGATION, BARAÚNA, RN

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