SoilNO3-storage from oasis development in deserts: Implications for the prevention and control of groundwater pollution

被引:4
|
作者
Qi, Shi [1 ]
Liu, Wei [2 ]
Shu, Heping [3 ]
Liu, Fei [4 ]
Ma, Jinzhu [5 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou, Peoples R China
[2] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Ecohydrol Inland River Basin, Lanzhou 730000, Peoples R China
[3] Lanzhou Univ, Coll Civil Engn & Mech, Key Lab Mech Disaster & Environm Western China, Minist Educ China, Lanzhou, Peoples R China
[4] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Key Lab Watershed Geog Sci, Nanjing, Peoples R China
[5] Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Minist Educ, Lanzhou, Peoples R China
关键词
desert; groundwater pollution; nitrate nitrogen; oasis development; stable isotope; LAND-USE CHANGE; VADOSE ZONE; RECHARGE; NITRATE; WATER; NITROGEN; CIRCULATION; MANAGEMENT; PLATEAU; CARBON;
D O I
10.1002/hyp.13855
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The sources and storage of soil NO(3)(-)in the western Tengger Desert, Northwest China, were explored using water chemistry analysis and stable isotope techniques. In line with the expansion and development of oases, part of the desert has been transformed into cultivated land and artificial forest land. The mean soil NO(3)(-)contents found in areas of cultivated land and artificial forest were 123.06 mg kg(-1)and 1.26 mg kg(-1), far higher and slightly lower than the background desert soil values, respectively. The delta N-15-NO(3)(-)and delta O-18-NO(3)(-)values in cultivated soils ranged from 1.00 to 11.81 parts per thousand, and from -1.85 to 8.99 parts per thousand, respectively, and the mean mNO(3)(-)/Cl(-)value in cultivated soils was 2.3. These figures would appear to demonstrate that the rapid increase in the nitrate content in soils is principally due to the use of nitrogen fertilizer. Such increases in soil NO(3)(-)storage is likely to promote the leaching of nitrogen into the groundwater where coarsely textured soils exist, the pollution of water sources used for irrigation water, and extreme precipitation events. The delta N-15-NO(3)(-)and delta O-18-NO(3)(-)values in groundwater ranged from 3.72 to 6.54 parts per thousand, and from -0.19 to 12.06 parts per thousand, respectively, mainly reflecting the nitrification of soil nitrogen. These values appeared similar to those measured in the soil water in adjacent areas of cultivated land and vegetated desert, indicating that the groundwater has been affected by both natural and artificial NO3-. Artificial afforestation of desert regions would therefore seem to be a useful way of reducing the threat posed by anthropogenic sources to the circulation of NO3--N within arid regions, as well as promoting wind sheltering and sand fixation. This study explored the NO(3)(-)storage and groundwater quality responses to oasis development in arid areas in an attempt to provide effective information for local agricultural organizations and agricultural nitrogen management models.
引用
收藏
页码:3941 / 3954
页数:14
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