Gao C, Zhu J G, Zhu J Y, Gao X, Dou Y J, Hosen Y
State Key Laboratory of Soil and Sustainable Agriculture (Institute of Soil Science, Chinese Academy of Sci), Nanjing 210008, PR China.
Environ Geochem Health. 2004 Jun-Sep;26(2-3):199-207. doi: 10.1023/b:egah.0000039582.68882.7f.
Temporal changes in nitrogen concentrations and stream discharge, as well as sediment and nitrogen losses from erosion plots with different land uses, were studied in an agricultural watershed in the Taihu Lake area in eastern China. The highest overland runoff loads and nitrogen losses were measured under the upland at a convergent footslope. Much higher runoff, sediment and nitrogen losses were observed under upland cropping and vegetable fields than that under chestnut orchard and bamboo forest. Sediment associated nitrogen losses accounted for 8-43.5% of total nitrogen export via overland runoff. N lost in dissolved inorganic nitrogen forms (NO(3-)-N + NH4+-N) accounted for less than 50% of total water associated nitrogen export. Agricultural practices and weather-driven fluctuation in discharge were main reasons for the temporal variations in nutrient losses via stream discharge. Significant correlation between the total nitrogen concentration and stream discharge load was observed. Simple regression models could give satisfactory results for prediction of the total nitrogen concentrations in stream water and can be used for better quantifying nitrogen losses from arable land. Nitrogen losses from the studied watershed via stream discharge during rice season in the year 2002 were estimated to be 10.5 kg N/ha using these simple models.
在中国东部太湖地区的一个农业流域,研究了不同土地利用方式下侵蚀地块中氮浓度、河流流量的时间变化,以及泥沙和氮的流失情况。在坡麓汇聚处的旱地,测得的地表径流负荷和氮流失量最高。与板栗园和竹林相比,旱地种植和菜地的径流、泥沙和氮流失量要高得多。与泥沙相关的氮流失占通过地表径流输出的总氮的8%-43.5%。以溶解无机氮形式(NO(3-)-N + NH4+-N)流失的氮占与水相关的总氮输出的不到50%。农业实践和流量的天气驱动波动是通过河流流量造成养分流失时间变化的主要原因。观察到总氮浓度与河流流量负荷之间存在显著相关性。简单回归模型可以为预测溪流水体中的总氮浓度给出令人满意的结果,并可用于更好地量化耕地的氮流失。利用这些简单模型估计,2002年水稻季该研究流域通过河流流量流失的氮为10.5 kg N/ha。