poster - International Conference of Agricultural Engineering
poster - International Conference of Agricultural Engineering poster - International Conference of Agricultural Engineering
Variability of water quality in a lake receiving drainage water from the Hetao irrigation system in the Yellow River basin, China Biao Sun 1 , Changyou Li 1 , Claudia M d S Cordovil 2 , Keli Jia 1 , Sheng Zhang 1 , Zhongyi Qu, Amarilis de Varennes 2 , and Luis S Pereira 2 1 College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot, 010018, PR China 2 CEER - Biosystems Engineering, Institute of Agronomy, Technical University of Lisbon, Tapada da Ajuda, 1349-017 Lisbon, Portugal * Email: lspereira@isa.utl.pt Abstract The Wuliangsuhai Lake is very important for the irrigation and drainage system of the Hetao Area in China. Between 2005 and 2010,water quality of the lake was monitored using physical, chemical and biological parameters. Chemical changes over time were not significant while COD was affected by the building of a new tomato plant as well as by a new Sewage Treatment Plant. To this day large amounts of organic industrial wastewaters are discharged into the lake without any treatment affecting water quality. Freezing of the lake during the cold season and flow direction affected several of the parameters monitored. Keywords: water quality dynamics, Irrigation, Wuliangsuhai Lake 1. Introduction Awareness of an impending water crisis began in the 1970’s but it was only in the 1990’s that water eutrophication became a serious problem in China (Jingan and Hongqing, 2002) affecting all economical activities dependent on freshwater quality. The Northwest of China is an arid or semi-arid region, depending on water for local economic development, namely water derived from the lakes. The Hetao Region is one of the three largest agricultural regions in China (Yang and Liu, 2002), with an irrigated area of about 5640 km 2 . Irrigation water comes mainly from the Yellow River (5 billion m 3 ) and is discharged into the Wuliangsuhai Lake (WL) (Fig. 1). In Hetao, pesticides and fertilizers were first used by the 1960’s. Rapid economic development led to an increase of urban wastewater discharge (0.5 billion m 3 ) and agricultural runoff into the WL from the upper channels (Wan, 2009). Currently, 1500 to 2000 tons of pesticides and 600000 tons of fertilizers are used per year (Liu, 2004), impacting the quality of thw WL water and compromising natural ecosystems. Groundwater quality of WL has been studied before (Liu et al., 2010) but little is known about surface water quality in the Hetao irrigation area. It is therefore urgent to identify polluting sources as well as the available practices to mitigate euthrophication of the lakes.
FIGURE 1. Location of the Wuliangsuhai Lake in Hetao 2 Materials and methods 2.1. Study area The WL is the largest in the Yellow River Basin in China, located between 108°43' and 108°57' E, and 40°36′ and 41°03′ N (0). It is about 35 to 40 km long, and 5 to 10 km wide, with a total area of 306 km 2 . A area of 177 km 2 is covered with reed and 129 km 2 is open water (Sun et al. 2011). The WL is very important for the irrigation and drainage system of Hetao area. The losses and discharges of wastewater from municipal and animal production sources, as well as losses from agricultural fields located around the lake, drain mainly into the Main Drainage Channel (90%). A net of irrigation channels connects the Main channel and WL (Fig. 1). The WL is frozen for about five months per year, usually from mid November to mid April. The WL capacity is about 0.33 billion m 3 and depth ranges from 0.5 to 3.0 m. Annual average air temperature is 7.3 ºC, with an average of 3185 hours of sunshine, 224 mm of annual rainfall, 1502 mm of evaporation per year and a 3.5 km h -1 wind speed. volume of irrigation water(10 9 m 3 ) 2,0 1,8 1,6 1,4 1,2 1,0 0,8 0,6 0,4 0,2 diverted for irrigation water discharged + surface drainage water 0,0 0,08 0,07 0,06 0,05 0,04 0,03 0,02 0,01 Jan. Apr. volume of discharge water(10 9 m 3 ) July Oct. 0,00 FIGURE 2. Average annual use of irrigation water in Hetao and discharge into WL.
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Variability <strong>of</strong> water quality in a lake receiving drainage water<br />
from the Hetao irrigation system in the Yellow River basin,<br />
China<br />
Biao Sun 1 , Changyou Li 1 , Claudia M d S Cordovil 2 , Keli Jia 1 , Sheng Zhang 1 ,<br />
Zhongyi Qu, Amarilis de Varennes 2 , and Luis S Pereira 2<br />
1 College <strong>of</strong> Water Conservancy and Civil <strong>Engineering</strong>, Inner Mongolia <strong>Agricultural</strong><br />
University, Hohhot, 010018, PR China<br />
2 CEER - Biosystems <strong>Engineering</strong>, Institute <strong>of</strong> Agronomy, Technical University <strong>of</strong> Lisbon,<br />
Tapada da Ajuda, 1349-017 Lisbon, Portugal<br />
* Email: lspereira@isa.utl.pt<br />
Abstract<br />
The Wuliangsuhai Lake is very important for the irrigation and drainage system <strong>of</strong> the<br />
Hetao Area in China. Between 2005 and 2010,water quality <strong>of</strong> the lake was monitored<br />
using physical, chemical and biological parameters. Chemical changes over time were<br />
not significant while COD was affected by the building <strong>of</strong> a new tomato plant as well as<br />
by a new Sewage Treatment Plant. To this day large amounts <strong>of</strong> organic industrial<br />
wastewaters are discharged into the lake without any treatment affecting water quality.<br />
Freezing <strong>of</strong> the lake during the cold season and flow direction affected several <strong>of</strong> the<br />
parameters monitored.<br />
Keywords: water quality dynamics, Irrigation, Wuliangsuhai Lake<br />
1. Introduction<br />
Awareness <strong>of</strong> an impending water crisis began in the 1970’s but it was only in the<br />
1990’s that water eutrophication became a serious problem in China (Jingan and<br />
Hongqing, 2002) affecting all economical activities dependent on freshwater quality. The<br />
Northwest <strong>of</strong> China is an arid or semi-arid region, depending on water for local<br />
economic development, namely water derived from the lakes. The Hetao Region is one<br />
<strong>of</strong> the three largest agricultural regions in China (Yang and Liu, 2002), with an irrigated<br />
area <strong>of</strong> about 5640 km 2 . Irrigation water comes mainly from the Yellow River (5 billion<br />
m 3 ) and is discharged into the Wuliangsuhai Lake (WL) (Fig. 1). In Hetao, pesticides<br />
and fertilizers were first used by the 1960’s. Rapid economic development led to an<br />
increase <strong>of</strong> urban wastewater discharge (0.5 billion m 3 ) and agricultural run<strong>of</strong>f into the<br />
WL from the upper channels (Wan, 2009). Currently, 1500 to 2000 tons <strong>of</strong> pesticides<br />
and 600000 tons <strong>of</strong> fertilizers are used per year (Liu, 2004), impacting the quality <strong>of</strong> thw<br />
WL water and compromising natural ecosystems. Groundwater quality <strong>of</strong> WL has been<br />
studied before (Liu et al., 2010) but little is known about surface water quality in the<br />
Hetao irrigation area. It is therefore urgent to identify polluting sources as well as the<br />
available practices to mitigate euthrophication <strong>of</strong> the lakes.