High concentrations of NO
3-, SO
42-, phosphate, and Al
3+ and low pH values were found in spring water which originated from a tea plantation. Although acidic spring water flowed into a local pond, the pH value of the pond water remained above 7 because of photosynthesis, denitrification and sulfate reduction. Photosynthesis caused by an increase of phosphate and NO
3- concentrations was concluded to have given rise to increases in pH values. Denitrification was thought to have caused the pond to eliminate NO
3- annually. Sulfate reduction was thought to have caused a disappearance of SO
42-. Phosphate was stored within a pond in the form of organic compounds. Al
3+ was precipitated within the pond because of increases in pH values.
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