This study presents an assessment of the quality of rainfall and runoff water, at the studied area based on analysis of three rainfall storms representing two consecutive years (2013 - 2014). The aim of this research paper was to identify whether the rainfall and runoff water quality had been influenced by the land use in Sulaimani governorate. The rainfall and runoff water quality were determined by comparing their chemical composition of major cations and anions with maximum permissible limits for water consumption and irrigation use. Analysis of PHreaction, temperature, electrical conducting, total dissolved solids, were done.Results showed that, values of electrical conductivity, total dissolved solids, took the highest values in forest land use for the first storms and took the highest values in asphalt land use in case of the two other storms. It also showed that the major ion contents show the trend Ca+2 > Mg+2 >K+>Na+ except asphalt land use where Na+ was more than K+, while anion composition follow the trend SO=4 > HCO-3>Cl-> NO=3>PO≡4 except asphalt land use where Cl- was more than HCO3-. The results appeared that the runoff water of the studied area are found to be unsuitable for domestic use according to Water Quality Index(WQI), while all runoff water samples from the studied land uses were suitable for the purpose of irrigation according to Irrigation water Quality Index,(IWQI).

Qalachwalan-Lesser Zab River receives varieties of domestic and chemical wastes from settlements, recreational and agricultural lands that located around the river. Those possibly affect the capacity of natural self-purification. Water samples have been collected from five different points between Qalachwalan to Qaladza district and sag curve were applied to analyzed water quality parameters for the periods of August 2016 to May 2017. The results showed that the dissolved oxygen values varied from 4.81 mg L -1 during August to 10.35 mg L -1 in February, biochemical oxygen demand values ranged from 1.47 mg L -1 during November to 8 mg L -1 in March along the river. The statistical analysis between predicted and measured dissolved oxygen and biochemical oxygen demand showed that the less value of root mean square errors was 1.09 mg L -1 for the month of April and the highest value was 3.92 mg L -1 for dissolved oxygen during May and the less value for biochemical oxygen demand was 0.77 mg L -1 for August and the highest value 5.08 mg L -1 for March. The predicted dissolved oxygen overestimated measured dissolved oxygen by percent bias 12.5% for April and 74.9% for May and the predicted biochemical oxygen demand overestimated measured biochemical oxygen demand as well by 23.4% for August and 98.9 % for February. The purification factor varied from 0.03 to 4.45 for all over the periods. The results, indicating that the river was temporarily polluted and has a poor capacity for self-purify particularly during April that the average factor was 0.14.