Zhu Anning, Zhang Jiabao, Zhao Bingzi, Cheng Zhuhua, Li Liping
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, People's Republic of China.
Environ Int. 2005 Aug;31(6):904-12. doi: 10.1016/j.envint.2005.05.038.
A 2-year field experiment was conducted in an Ochric Aquic Cambosols on a 1-ha field with rotation of winter wheat-summer corn located in Fengqiu County in North China Plain from 1 October 1998 to 30 September 2000 to quantify water balance and evaluate soil water loss by deep drainage and nitrate loss by leaching out of the root zone under the current agricultural practices. Considerable deep drainage was found especially in 1999-2000, during which period up to 273.9 mm of water, accounting for 60.6% of total amount of irrigation and 24.7% of total surface input (rainfall+irrigation), was lost by deep drainage. Even in both wheat cropping seasons when total amount of surface input was less than total actual evapotranspiration, 84.0 and 121.3 mm water was lost by drainage in 1999 and 2000, respectively. Soil NO3(-)-N was transported to deeper soil layers during the growing seasons and considerable amount of NO3(-)-N accumulated at 170 cm soil layer (the bottom of root zone) during the September-October period (the harvest time of summer corn) every year. About 28.6 kg N ha-1 was lost by leaching out of the root zone in 1998-1999 and 81.8 kg N ha-1 in 1999-2000, accounting for 5.9% and 15.7% of total nitrogen (N) inputs, respectively. The significant deep drainage and nitrate leaching loss were attributed to excessive and inappropriate irrigation and nitrogen (N) fertilization, which may result in severe groundwater pollution if current agricultural managements are not changed.
1998年10月1日至2000年9月30日,在中国华北平原封丘县一块1公顷的农田上,开展了一项为期两年的田间试验。该农田为潮土,种植模式为冬小麦-夏玉米轮作,目的是量化水分平衡,并评估当前农业生产方式下深层排水造成的土壤水分流失以及根区淋溶导致的硝态氮损失。结果发现,深层排水量相当可观,尤其是在1999-2000年期间,该时段深层排水量达273.9毫米,占灌溉总量的60.6%,占地表总输入量(降雨+灌溉)的24.7%。即使在两个小麦种植季,地表总输入量小于实际蒸散总量时,1999年和2000年分别仍有84.0毫米和121.3毫米的排水量。在作物生长季,土壤硝态氮向深层土壤层运移,每年9-10月(夏玉米收获期),在170厘米土层(根区底部)积累了大量硝态氮。1998-1999年和1999-2000年,根区淋溶损失的氮分别约为28.6千克/公顷和81.8千克/公顷,分别占总氮输入量的5.9%和15.7%。深层排水和硝态氮淋溶损失显著,是由于过度和不合理的灌溉及氮肥施用所致。如果不改变当前的农业管理方式,可能会导致严重的地下水污染。