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Groundwater quality monitoring for agriculture irrigated in Catol Do Rocha, Paraba State, Brazil
Author(s) -
Franklin Mesquita Evandro,
Ferreira Cavalcante Lourival,
Francisco Thiago Coelho Bezerra,
Mesquita Alves Jackson,
Thyago Aires Souza Jose,
Caio da Silva Sousa,
Gustavo Antônio,
Araújo de Lima Danila
Publication year - 2018
Publication title -
african journal of agricultural research
Language(s) - English
Resource type - Journals
ISSN - 1991-637X
DOI - 10.5897/ajar2018.13429
Subject(s) - sodium adsorption ratio , irrigation , potassium , salinity , sodium , arid , water quality , soil salinity , environmental science , groundwater , environmental chemistry , chemistry , soil water , zoology , hydrology (agriculture) , agronomy , soil science , geology , biology , ecology , geotechnical engineering , organic chemistry , drip irrigation
The electrical conductivity and of cations (Ca2+, Mg2+, Na+ and K+) and anions (Cl-, CO32-, HCO3- and SO42) contents of the water an Amazon well, from State University of Paraiba, Catole do Rocha city, Paraiba State, Brazil, located in the semi-arid region of the Brazilian High Sertao were evaluated monthly from January to December of year 2017. Despite the increase in electrical conductivity from 0.89 to 1.16 mS cm-1 and sodium adsorption ratio (SAR) from 4.43 to 10.45 (mmol L-1)1/2 did not change the water quality to agriculture. With mean risk to saline (C2) and low risk to exercise sodicity at soil (S1), toxicity and nutritional imbalance to plants, the concentration of dissolved salts increased from 0.57 to 0.74 g L-1 between rainy and arid periods. This situation expresses a high increase of almost 30% in the total dissolved salts during the evaluated period and shows the need for systematic monitoring. Simulating the irrigation with a 400 mm blade of this water with 1.16 dS m-1, in 120 days, can add to soil 2,970 kg ha-1 of salts, of which 1,892; 633; 258 and 143 kg ha-1 are of the sodium, calcium, potassium and magnesium species, respectively. Key words: Water quality, ionic components of water, salinity of water in well.

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