Monitoring the Hydrogen Potential of a River in the Central Andes of Peru From the Cloud
			
	
 
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				Universidad Nacional de Huancavelica, Facultad de Ingeniería Electrónica-Sistemas, Jr. La Mar N° 755, Pampas-Tayacaja, Huancavelica, Perú
				 
			 
						
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				Universidad Nacional del Centro del Perú, Unidad de Postgrado de la Facultad de Ciencias Forestales y del Ambiente, Av. Mariscal Castilla N° 3909-4089, Huancayo, Perú
				 
			 
										
				
				
		
		 
			
			
		
		
		
		
		
			
			 
			Data publikacji: 01-11-2021
			 
		 			
		 
	
							
					    		
    			 
    			
    				    					Autor do korespondencji
    					    				    				
    					Hipólito  Carbajal Morán   
    					Universidad Nacional de Huancavelica, Facultad de Ingeniería Electrónica-Sistemas, Jr. La Mar N° 755, Pampas-Tayacaja, Huancavelica, Perú
    				
 
    			
				 
    			 
    		 		
			
																						 
		
	 
		
 
 
Ecol. Eng. Environ. Technol. 2021; 6:17-26
		
 
 
SŁOWA KLUCZOWE
DZIEDZINY
STRESZCZENIE
The hydrogen potential is one of the parameters of the water which is variable in rivers throughout their journey over the cities, so the objective of the work was to monitor (from the cloud) the pH of the Upamayu river waters (Huancavelica region), located in the Central Andes of Peru. An electronic system was implemented, comprising: DS18B20 temperature sensor, 4502C pH sensor, ESP32 controller, NEO 6M GPS global positioning system, LabVIEW NXG platform, in addition to the web server developed in ThingSpeak. The measurements were established under the protocol for water resources of Peru. As a result, a pH monitoring system of the waters of the river under study was verified. Through the sensors, it takes the data and sends them to the web server located in the cloud via the implemented algorithm. The data read from any remote place through an application implemented in LabVIEW NXG, representing the monitoring station on a GIS map. It was concluded that the values of the hydrogen potential are different in relation to its territorial distribution and in the dry season. Varying pH after the discharge of polluting sources of the population and the places of cattle raising was found; likewise, regeneration of the waters at a certain distance was shown.