10.11.2014 Views

poster - International Conference of Agricultural Engineering

poster - International Conference of Agricultural Engineering

poster - International Conference of Agricultural Engineering

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

3.2. Variability <strong>of</strong> parameters<br />

The spatial distribution <strong>of</strong> the overall means <strong>of</strong> measured parameters is shown in Fig.<br />

4. The greatest values for temperature, electrical conductivity, pH and dissolved<br />

organics was measured in the south <strong>of</strong> the lake in agreement with the direction <strong>of</strong> the<br />

water flow, from northeast to southwest. Totals <strong>of</strong> N and P were higher near the<br />

entrance <strong>of</strong> the channels which discharge into the WL (Fig 4.). COD and Chl.a are very<br />

consistent in this spatial distribution, thus revealing the discharge <strong>of</strong> wastewater into the<br />

WL. Nitrogen and P consumption by reed which covers about 15% <strong>of</strong> the lake might<br />

explain the decrease in the concentrations along the flow.<br />

4. Conclusions<br />

The main factors influencing temporal variations in water quality seem to be<br />

agricultural losses <strong>of</strong> nutrients as well as wastewater discharge into the channels which<br />

lead into the WL. Winter seems to be the season where the water has a greater load <strong>of</strong><br />

nutrients and evaporation during summer may influence parameters concentration. The<br />

direction <strong>of</strong> water flow and the position <strong>of</strong> channels in and out <strong>of</strong> the WL also influenced<br />

the concentration <strong>of</strong> parameters concentration in the water.<br />

Acknowledgments<br />

We would like to thank the lake research team in Inner Mongolia <strong>Agricultural</strong><br />

University for their persistent efforts in collecting/measuring the data in this study. The<br />

study is supported by the Sino-Portuguese cooperative research project, MOST, China,<br />

and FCT, Portugal .<br />

Reference list<br />

Ma, J. & Li, H. (2002). Preliminary discussion on eutrophication status <strong>of</strong> lakes,<br />

reservoirs and rivers in China and overseas. Resources and Environment in the<br />

Yangtze Basin 6, 575-578 (in Chinese).<br />

Yang, L. & Liu, Y. (2002). Discussion on water resources utilization in Hetao Irrigation<br />

District in Inner Mongolia Autonomous Region. Proceedings <strong>of</strong> agricultural engineering<br />

science and technology, 128-130.<br />

Liu, Z. (2004). Research about estimation the input to the lake Wuliangsuhai from farmland<br />

surface pollution. Inner Mongolia university Master Degree Thesis, 14-33 (in Chinese).<br />

Wan, F. (2009). Study on Ecological Water Supplement <strong>of</strong> Wu Liang Su Lake. Xi'an<br />

University <strong>of</strong> Technology Master Degree Thesis, 10-41 (in Chinese).<br />

Liu, W., Gao, C., Liu B. & Chen, Y. (2010). Hydro-chemical constituents and correlation<br />

analysis <strong>of</strong> shallow groundwater in the Hetao Plain. Geology in China 37, 816-823 (in<br />

Chinese).<br />

Qu, Z.Y., Chen, Y.X., Shi, H.B., Wei, Z.M., Li, Y.L. & Zhang, Y.Q. (2003). Regional<br />

groundwater depth forecast by BP model <strong>of</strong> post-water-saving reconstruction in the<br />

Hetao Irrigation District <strong>of</strong> Inner Mongolia. Trans. CSAE 19 (1), 59–62 (in Chinese).<br />

Xu X, Huang GH, Qu ZY & Pereira LS (2010) Assessing the groundwater dynamics<br />

and predicting impacts <strong>of</strong> water saving in the Hetao Irrigation District, Yellow River basin.<br />

Agric. Water Manage 98, 301-313

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!