Source of nitrogen in wet deposition to a rice agroecosystem at Tai lake region

Abstract

Nitrogen (N) in wet deposition can provide significant nutrients to algae, which potentially contributes to eutrophication in waterbodies, and to nutrient surplus of rice–wheat crops in the Tai lake region, Jiangsu Province, China. Quantifying the N compounds in wet deposition and determining their sources is important to understand how to control eutrophication in lakes and to improve recommendations for fertilizer use. In this study, the concentrations of inorganic N, molar ratios of NH 4 +/NO 3 − and the natural 15N abundance of NH 4 + ( δ 15NH 4 +) in wet deposition were determined for 78 precipitation events between June 2003 and July 2005. Samples were collected at two sites in Tai lake region, a watershed rice agroecosystem currently experiencing eutrophication. The average N wet deposition amounted to 27 kg N ha −1 yr −1, with 60% in the form of NH 4 +. Annually, two cycles of depleted and enriched δ 15NH 4 + indicate the shifting of main source of NH 3 volatilization between chemical fertilizer and excreta of local residents and domestic animals, surface waters, and other organic N. The peak in NH 4 +/NO 3 − ratio, coupled with depleted δ 15NH 4 + in mid-June, coincided with the rice-transplanting period, which is indicative of surplus fertilizer application. Enriched δ 15NH 4 + values in August–October and in April–May were indicative of enhanced emissions from excreta and polluted waterbodies in the warmer seasons. Findings suggest that δ 15NH 4 + could be used to indicate the sources of NH 3 volatilization, and the NH 4 +/NO 3 − ratio to indicate the intensity of wet N deposition.