2020 Volume 39 Issue 8
Article Contents

HE Liping, LAN Bo, LU Wei, DUAN Linyan, LIN Junjie. Transformation process of purple alluvial soil combined nitrogen in water level fluctuation zone of the Three Gorges Reservoir Area[J]. Environmental Chemistry, 2020, (8): 2245-2252. doi: 10.7524/j.issn.0254-6108.2019091704
Citation: HE Liping, LAN Bo, LU Wei, DUAN Linyan, LIN Junjie. Transformation process of purple alluvial soil combined nitrogen in water level fluctuation zone of the Three Gorges Reservoir Area[J]. Environmental Chemistry, 2020, (8): 2245-2252. doi: 10.7524/j.issn.0254-6108.2019091704

Transformation process of purple alluvial soil combined nitrogen in water level fluctuation zone of the Three Gorges Reservoir Area

  • Corresponding author: LIN Junjie, ybu_lin@126.com
  • Received Date: 17/09/2019
    Fund Project: Supported by the Science and Technology Research Program of Chongqing Municipal Education Commission (KJ1710260, KJQN201801233, KJZD-K201801201, KJQN20181230), the Program of Chongqing Science and Technology Commission (cstc2018jcyjAX0813), the Chongqing Municipal Key Laboratory of Institutions of Higher Education (WEPKL2016LL-03) and Sustainable Development Research Centre of Three Gorges Reservoir Area (18sxxyjd11).
  • The transformation process of soil combined nitrogen (N) is an essential factor, which affects N release from the soil of water level fluctuation (WLF) zone to the surrounding water body. Therefore, purple alluvial soils in the WLF zone of Three Gorges Reservoir Area were collected for the discussion of the above scientific problem in an incubation experiment. The results showed that during aerobic and anaerobic incubation of 0-3 days, soil N of ion-exchangeable form (IEF-N) content increased by 20.85 mg·kg-1 and 28.78 mg·kg-1, respectively. Meanwhile, soil N of iron-manganese oxides form (IMOF-N) content decreased by 30.04 mg·kg-1 and 31.49 mg·kg-1, respectively; Soil N of organic matter-sulfide form (OSF-N) content decreased by 84.63 mg·kg-1 and 95.38 mg·kg-1, respectively. Besides, IMOF-N and OSF-N content significantly correlated with IEF-N content during aerobic and anaerobic incubation. In summary, IMOF-N and OSF-N partly (lower than 25%) transformed to IEF-N during aerobic and anaerobic incubation of 0-3 days. Thus, compared with the other period, the N release risk in purple alluvial soil was much higher during the dry and flooding periods of 0-3 days in the WLF zone. The results were helpful for accurately assessing the risk of N release from the soil of WLF zone to the Three Gorges Reservoir.
  • 加载中
  • [1] BAO Y, GAO P, HE X. The water-level fluctuation zone of Three Gorges Reservoir-A unique geomorphological unit[J]. Earth-Science Reviews, 2015, 150:14-24.

    Google Scholar Pub Med

    [2] 林俊杰, 刘丹, 张帅, 等. 淹水-落干与季节性温度升高耦合过程对消落带沉积物氮矿化影响[J]. 环境科学, 2017, 38(2):555-562. LIN J, ZHEN D, ZHANG S, et al. Effect of coupling process of wetting-drying cycles and seasonal temperature increasing on sediment nitrogen mineralization in the water level fluctuating zone[J]. Environmental Science, 2017, 38(2):555-562(in Chinese).

    Google Scholar Pub Med

    [3] JIANG Q, XU Z, HAO Y, et al. Dynamics of soil labile carbon and nitrogen pools in riparian zone of Wyaralong Dam in Southeast Queensland, Australia[J]. Journal of Soils and Sediments, 2017, 17(4):1030-1044.

    Google Scholar Pub Med

    [4] ZHANG A, CORNWELL W, LI Z, et al. Dam effect on soil nutrients and potentially toxic metals in a reservoir riparian zone[J]. Clean-Soil, Air, Water, 2019, 47(1):1700497.

    Google Scholar Pub Med

    [5] YANG Z, LIU D, JI D, et al. Influence of the impounding process of the Three Gorges Reservoir up to water level 172.5 m on water eutrophication in the Xiangxi Bay[J]. Science China Technological Sciences, 2010, 53(4):1114-1125.

    Google Scholar Pub Med

    [6] YE L, HAN X, XU Y, et al. Spatial analysis for spring bloom and nutrient limitation in Xiangxi Bay of Three Gorges Reservoir[J]. Environmental Monitoring and Assessment, 2007, 127(1-3):135-145.

    Google Scholar Pub Med

    [7] MARIANO E, JONES D L, HILL P W, et al. Mineral nitrogen forms alter 14C-glucose mineralization and nitrogen transformations in litter and soil from two sugarcane fields[J]. Applied Soil Ecology, 2016, 107:154-161.

    Google Scholar Pub Med

    [8] NIEDER R, BENBI D K, SCHERER H W. Fixation and defixation of ammonium in soils:A review[J]. Biology and Fertility of Soils, 2011, 47(1):1-14.

    Google Scholar Pub Med

    [9] LIU Y L, ZHANG B, LI C L, et al. Long-term fertilization influences on clay mineral composition and ammonium adsorption in a rice paddy soil[J]. Soil Science Society of America Journal, 2008, 72(6):1580-1590.

    Google Scholar Pub Med

    [10] 刘波, 周锋, 王国祥, 等. 沉积物氮形态与测定方法研究进展[J]. 生态学报, 2011, 31(22):6947-6958. LIU B, ZHOU F, WANG G X, et al. Research progress on forms of nitrogen and determination in the sediments[J]. Acta Ecologica Sinica, 2011, 31(22):6947-6958(in Chinese).

    Google Scholar Pub Med

    [11] 马红波, 宋金明, 吕晓霞, 等. 渤海沉积物中氮的形态及其在循环中的作用[J]. 地球化学, 2003, 32(1):48-54. MA H B, SONG J M, LÜ X X, et al. Nitrogen forms and their functions in recycling of the Bohai Sea sediments[J]. Geochimica, 2003, 32(1):48-54(in Chinese).

    Google Scholar Pub Med

    [12] LI X, HOU L, LIU M, et al. Evidence of nitrogen loss from anaerobic ammonium oxidation coupled with ferric iron reduction in an intertidal wetland[J]. Environmental Science and Technology, 2015, 49(19):11560-11568.

    Google Scholar Pub Med

    [13] DING L J, AN X L, LI S, et al. Nitrogen loss through anaerobic ammonium oxidation coupled to iron reduction from paddy soils in a chronosequence[J]. Environmental Science and Technology, 2014, 48(18):10641-10647.

    Google Scholar Pub Med

    [14] 杨杰,夏品华,林陶, 等.贵州草海湿地不同水深梯度下沉积物铁形态分布特征[J]. 环境化学, 2019, 38(4):813-821. YANG J, XIA P H, LIN T, et al. Distribution characteristics of iron speciation in sediments of Guizhou Caohai wetland under different water depths[J]. Environmental Chemistry, 2019, 38(4):813-821(in Chinese).

    Google Scholar Pub Med

    [15] LIU Y, WANG C, HE N, et al. A global synthesis of the rate and temperature sensitivity of soil nitrogen mineralization:Latitudinal patterns and mechanisms[J]. Global Change Biology, 2017, 23(1):455-464.

    Google Scholar Pub Med

    [16] OSTERHOLZ W R, RINOT O, LIEBMAN M, et al. Can mineralization of soil organic nitrogen meet maize nitrogen demand?[J]. Plant and Soil, 2017, 415(1-2):73-84.

    Google Scholar Pub Med

    [17] REUSSI C N, WYNGAARD N, ORCELLET J, et al. Predicting field-apparent nitrogen mineralization from anaerobically incubated nitrogen[J]. Soil Science Society of America Journal, 2018, 82(2):502-508.

    Google Scholar Pub Med

    [18] XU X, HUI D, KING A W, et al. Convergence of microbial assimilations of soil carbon, nitrogen, phosphorus, and sulfur in terrestrial ecosystems[J]. Scientific Reports, 2015, 5:17445.

    Google Scholar Pub Med

    [19] 张彬, 陈猷鹏, 方芳, 等.三峡库区淹没消落区土壤氮素形态及分布特征[J]. 环境科学学报, 2012, 32(5):1126-1133. ZHANG B, CHEN Y P, FANG F, et al. Nitrogen forms and their distribution characteristics in the soils of water level fluctuation zone in the central Three Gorges Reservoir[J]. Acta Scientiae Circumstantiae, 2012, 32(5):1126-1133(in Chinese).

    Google Scholar Pub Med

    [20] 张雷, 秦延文, 郑丙辉, 等. 三峡入库河流大宁河回水区浸没土壤及消落带土壤氮形态及分布特征[J]. 环境科学, 2009, 30(10):2884-2890. ZHANG L, QIN Y W, ZHENG B H, et al. Nitrogen forms and its distribution character in immerged and water-level fluctuating zone soils of the backwater reach from input river of Three Gorges Reservoir[J]. Environmental Science, 2009, 30(10):2884-2890(in Chinese).

    Google Scholar Pub Med

    [21] 何立平, 刘丹, 于志国, 等. 三峡库区干支流落干期消落带土壤可转化态氮含量及分布特征[J]. 环境科学, 2016, 37(3):950-954. HE L P, LIU D, YU Z G, et al. Distribution and content of transferable nitrogen in the soil of water level fluctuating zones of mainstream and its tributaries of Three Gorges Reservoir Areas during the dry period[J]. Environmental Science, 2016, 37(3):950-954(in Chinese).

    Google Scholar Pub Med

    [22] 林俊杰, 张帅, 杨振宇, 等. 干湿循环对三峡支流消落带沉积物中可转化态氮及其形态分布的影响[J]. 环境科学, 2015, 36(7):2459-2464. LIN J J, ZHANG S, YANG Z Y, et al. Effect of drought and subsequent re-wetting cycles on transferable nitrogen and Its form distribution in the sediment of water level fluctuating zone in the tributary of Three Gorge Reservoir Areas[J]. Environmental Science, 2015, 36(7):2459-2464(in Chinese).

    Google Scholar Pub Med

    [23] 王晓锋, 袁兴中, 刘红,等. 三峡库区消落带4种典型植物根际土壤养分与氮素赋存形态[J]. 环境科学, 2015, 36(10):3662-3673. WANG X F, YUAN X Z, LIU H, et al. Nutrient characteristics and nitrogen forms of rhizosphere soils under 4 typical plants in the littoral zone of TGR[J]. Environmental Science, 2015, 36(10):3662-3673(in Chinese).

    Google Scholar Pub Med

    [24] BLAGODATSKAYA E, YUYUKINA T, BLAGODATSKY S, et al. Turnover of soil organic matter and of microbial biomass under C3-C4 vegetation change:Consideration of 13C fractionation and preferential substrate utilization[J]. Soil Biology & Biochemistry, 2011, 43(1):159-166.

    Google Scholar Pub Med

    [25] 袁从禕. 土壤机械组成的比重计速测法[J]. 土壤通报, 1964, 1(5):1-3. YUAN C W. Rapid determination method of soil mechanical composition[J]. Chinese Journal of Soil Science, 1964, 1(5):1-3(in Chinese).

    Google Scholar Pub Med

    [26] 王虹, 崔桂霞. 用氯化钡缓冲液法测定土壤阳离子交换量[J]. 土壤, 1989, 21(1):49-51. WANG H, CUI G X. The determination of soil cation exchange capacity by the method of Barium chloride buffer solution[J]. Soil, 1989, (1):49-51(in Chinese).

    Google Scholar Pub Med

    [27] JANSSEN B H. Nitrogen mineralization in relation to C:N ratio and decomposability of organic materials, Progress in Nitrogen Cycling Studies[M]. Berlin:Springer, 1996:69-75.

    Google Scholar Pub Med

    [28] GHALY A, RAMAKRISHNAN V. Nitrogen sources and cycling in the ecosystem and its role in air, water and soil pollution:A critical review[J]. Journal of Pollution Effects and Control, 2015, 3(2):1-26.

    Google Scholar Pub Med

    [29] WANG S, RADNY D, HUANG S, et al. Nitrogen loss by anaerobic ammonium oxidation in unconfined aquifer soils[J]. Scientific Reports, 2017, 7:40173.

    Google Scholar Pub Med

    [30] WU J, HONG Y, HE X, et al. Anaerobic ammonium oxidation in acidic red soils[J]. Frontiers in Microbiology, 2018, 9:2142.

    Google Scholar Pub Med

    [31] BAO P, LI G X. Sulfur-driven iron reduction coupled to anaerobic ammonium oxidation[J]. Environmental Science and Technology, 2017, 51(12):6691-6698.

    Google Scholar Pub Med

    [32] MOGOLLÓN J M, MEWES K, KASTEN S. Quantifying manganese and nitrogen cycle coupling in manganese-rich, organic carbon-starved marine sediments:Examples from the Clarion-Clipperton fracture zone[J]. Geophysical Research Letters, 2016, 43(13):7114-7123.

    Google Scholar Pub Med

    [33] LIU S, LIN F, WU S, et al. A meta-analysis of fertilizer-induced soil NO and combined NO+ N2O emissions[J]. Global Change Biology, 2017, 23(6):2520-2532.

    Google Scholar Pub Med

    [34] GUGGENBERGER G. Humification and mineralization in soils, microorganisms in soils:Roles in genesis and functions[M]. Berlin:Springer, 2005:85-106.

    Google Scholar Pub Med

    [35] OSTERHOLZ W R, RINOT O, SHAVIV A, et al. Predicting gross nitrogen mineralization and potentially mineralization nitrogen using soil organic matter properties[J]. Soil Science Society of America Journal, 2017, 81(5):1115-1126.

    Google Scholar Pub Med

    [36] ZHAO Q, POULSON S R, OBRIST D, et al. Iron-bound organic carbon in forest soils:Quantification and characterization[J]. Biogeosciences, 2016, 13(16):4777-4788.

    Google Scholar Pub Med

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(1069) PDF downloads(22) Cited by(0)

Access History

Transformation process of purple alluvial soil combined nitrogen in water level fluctuation zone of the Three Gorges Reservoir Area

Fund Project: Supported by the Science and Technology Research Program of Chongqing Municipal Education Commission (KJ1710260, KJQN201801233, KJZD-K201801201, KJQN20181230), the Program of Chongqing Science and Technology Commission (cstc2018jcyjAX0813), the Chongqing Municipal Key Laboratory of Institutions of Higher Education (WEPKL2016LL-03) and Sustainable Development Research Centre of Three Gorges Reservoir Area (18sxxyjd11).

Abstract: The transformation process of soil combined nitrogen (N) is an essential factor, which affects N release from the soil of water level fluctuation (WLF) zone to the surrounding water body. Therefore, purple alluvial soils in the WLF zone of Three Gorges Reservoir Area were collected for the discussion of the above scientific problem in an incubation experiment. The results showed that during aerobic and anaerobic incubation of 0-3 days, soil N of ion-exchangeable form (IEF-N) content increased by 20.85 mg·kg-1 and 28.78 mg·kg-1, respectively. Meanwhile, soil N of iron-manganese oxides form (IMOF-N) content decreased by 30.04 mg·kg-1 and 31.49 mg·kg-1, respectively; Soil N of organic matter-sulfide form (OSF-N) content decreased by 84.63 mg·kg-1 and 95.38 mg·kg-1, respectively. Besides, IMOF-N and OSF-N content significantly correlated with IEF-N content during aerobic and anaerobic incubation. In summary, IMOF-N and OSF-N partly (lower than 25%) transformed to IEF-N during aerobic and anaerobic incubation of 0-3 days. Thus, compared with the other period, the N release risk in purple alluvial soil was much higher during the dry and flooding periods of 0-3 days in the WLF zone. The results were helpful for accurately assessing the risk of N release from the soil of WLF zone to the Three Gorges Reservoir.

Reference (36)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint