Nitrogen wet deposition was monitored for two years (2001.6-2003.5) at the Changshu Ecological Station in Taihu Lake region. The results showed that the amount of nitrogen wet deposition had a strong seasonal pattern, with higher levels in summer and spring, and low values in autumn and winter. The proportions of NH4(+)-N, NO3(-)-N and DON (dissolved organic nitrogen) to TN (total nitrogen) inputted by wet deposition were 47.6%, 35.1% and 17.4%, respectively. Ammonia volatilization from farmland was the most important source of NH4(+)-N in wet deposition. The monthly NH4(+)-N input from wet deposition increased with monthly rainfall (R2 = 0.3178**), while the monthly NO3(-)-N input from wet deposition had a lower correlation (R2 = 0.1985*) with monthly rainfall but positively related with the time of rainfall (R2 = 0.6757***). The NO3(-)-N concentration in the air was relatively steady in a period of time. Its concentration in wet deposition had a negative correlation with rainfall (R2 = 0.4205***). The annual TN input from wet deposition was 27.0 kg x hm(-2), but its concentration in each rainfall was higher than 0.2 mg x L(-1) (the threshold N concentration for inland water eutrophication). The nitrogen inputted by wet deposition had an ecological significance on both nitrogen balance in agroecosystem and eutrophication.
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ACS Omega
January 2025
School of Ecology and Environment, Renmin University of China, No.59 Zhongguancun Street, Beijing 100872, China.
Hydrothermal liquefaction (HTL) is a promising technology for converting wet biomass to liquid fuels. However, the biocrude yield and quality in this process are unsatisfactory without catalysts. Herein, a Ru/ZrO-SiO catalyst was prepared with the NaBH reducing method for the HTL of .
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Department of Pharmacy Practice, Faculty of Pharmacy, Airlangga University, Surabaya, Indonesia.
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CNR-IGG Institute of Geosciences and Earth Resources, Via La Pira 4, 50121 Florence, Italy.
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