Su Yong-Zhong, Yang Xiao, Yang Rong
Huan Jing Ke Xue. 2014 Oct;35(10):3683-91.
In irrigated agricultural ecosystems, the accumulation, distribution and transfer of nitrate nitrogen (NO(3-)-N) in soil profile and groundwater nitrate pollution were influenced by irrigation and fertilization, and were closely related to soil textural characteristics. In this study, a monitoring section with 10 groundwater observation wells along Heihe River flood land-old oasis croplands-newly cultivated sandy croplands-fixed sandy land outside oasis was established in Pingchuan desert-oasis in Linze county in the middle of Heihe river basin, and groundwater NO(3-)-N concentration was continuously monitored. Soil texture and NO(3-)-N concentration in the unsaturated zone at different landscape locations were determined. The NO(3-)-N transfer change in soil profile, nitrate leaching of soils with different texture and fertility levels in the 0-100 cm layer were analyzed. The results indicated that the vertical distribution of soil texture was sandy loam in the 0-130 cm depth, loam in the 130-190 cm and clay loam in the 190-300 cm for the old oasis croplands. For newly cultivated sandy croplands, sand content was more than 80% in each soil layer of the 0-300 cm profile, although a thin clay layer occurred in the 140-160 cm depth. The clay layer occurred 160 cm below the sand-fixing zone outside oasis. There were significant correlations between soil NO(3-)-N concentration and silt + clay content, and the order of significant degree was the natural soils of sandy lands > the newly cultivated sandy croplands > the old oasis croplands. The loss of N leaching was closely correlated to the silt + caly content in the 0-100 cm soil depth. The groundwater NO(3-)-N concentration varied from 1.01 to 5.17 mg · L(-1), with a mean value of 2.65 mg · L(-1) and from 6.6 to 29.5 mg · L(-1), with an average of 20.8 mg · L(-1) in the area of old oasis croplands and the newly cultivated croplands, respectively. The averaged groundwater NO(3-)-N concentration in the area of newly cultivated sandy croplands during the period of May and October, 2013 was 26.5 mg · L(-1), which was increased by 9.5 mg · L(-1) in comparison with the same period of 2012. There was a clear increasing trend in groundwater NO(3-)-N concentration in the sand-fixing zone outside oasis. The textural characteristics of soil unsaturated zone in the shallow groundwater distribution area was the key determining factor for controlling soil NO(3-)-N leaching and groundwater nitrate pollution. The newly cultivated sandy croplands were the nitrate vulnerable zones and high-risk areas of groundwater nitrate pollution. The implementation of cultivation pattern and irrigation and fertilization management that could effectively reduce groundwater NO(3-)-N pollution should be considered in the development of ecological agriculture.
在灌溉农业生态系统中,土壤剖面中硝态氮(NO₃⁻-N)的积累、分布和迁移以及地下水硝酸盐污染受灌溉和施肥影响,且与土壤质地特征密切相关。本研究在黑河中游临泽县平川荒漠绿洲,沿黑河漫滩-老绿洲农田-新垦沙地农田-绿洲外固定沙地设置了一个包含10口地下水观测井的监测断面,持续监测地下水NO₃⁻-N浓度。测定了不同景观位置非饱和带土壤质地和NO₃⁻-N浓度。分析了土壤剖面中NO₃⁻-N迁移变化、0-100 cm土层不同质地和肥力水平土壤的硝酸盐淋失情况。结果表明,老绿洲农田0-130 cm深度土壤质地为砂壤土,130-190 cm为壤土,190-300 cm为粘壤土。新垦沙地农田0-300 cm剖面各土层砂含量均超过80%,仅在140-160 cm深度有一层薄粘土层。绿洲外固定沙地粘土层出现在固沙带以下160 cm处。土壤NO₃⁻-N浓度与粉粒+粘粒含量显著相关,显著程度顺序为沙地天然土壤>新垦沙地农田>老绿洲农田。0-100 cm土壤深度氮淋失量与粉粒+粘粒含量密切相关。老绿洲农田区和新垦农田区地下水NO₃⁻-N浓度分别在1.01至5.17 mg·L⁻¹之间,平均值为2.65 mg·L⁻¹,以及在6.6至29.5 mg·L⁻¹之间,平均为20.8 mg·L⁻¹。2013年5月至10月期间,新垦沙地农田区地下水NO₃⁻-N平均浓度为26.5 mg·L⁻¹,比2012年同期增加了9.5 mg·L⁻¹。绿洲外固沙带地下水NO₃⁻-N浓度呈明显上升趋势。浅层地下水分布区土壤非饱和带质地特征是控制土壤NO₃⁻-N淋失和地下水硝酸盐污染的关键决定因素。新垦沙地农田是地下水硝酸盐污染的硝酸盐易损区和高风险区。生态农业发展应考虑实施能有效减少地下水NO₃⁻-N污染的种植模式及灌溉施肥管理措施。