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Soil NO 3 − storage from oasis development in deserts: Implications for the prevention and control of groundwater pollution
Author(s) -
Qi Shi,
Liu Wei,
Shu Heping,
Liu Fei,
Ma Jinzhu
Publication year - 2020
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/hyp.13855
Subject(s) - soil water , groundwater , leaching (pedology) , environmental science , nitrate , irrigation , hydrology (agriculture) , fertilizer , environmental chemistry , soil science , agronomy , ecology , chemistry , geology , geotechnical engineering , biology
Abstract 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 δ 15 N‐NO 3 − and δ 18 O‐NO 3 − values in cultivated soils ranged from 1.00 to 11.81 ‰, and from −1.85 to 8.99 ‰, 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 δ 15 N‐NO 3 − and δ 18 O‐NO 3 − values in groundwater ranged from 3.72 to 6.54 ‰, and from −0.19 to 12.06 ‰, 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 NO 3 − . 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 NO 3 − ‐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.