Original Articles

The Application of Radiocarbon in the Study of Soil Carbon Cycles

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  • 1. Institute of Gegographical Sciences and Natural Resources Research, CAS, Beijing 100101;
    2. Graduate School of CAS, Beijing 100039

Received date: 2004-01-01

  Revised date: 2004-03-01

  Online published: 2004-07-24

Abstract

The carbon cycles in the soil is important for the study of the global change because the carbon deposited in the soil is two times more than that in the atmosphere and three times more than that in the plant and animal. While the final mechanism of the terrestrial carbon cycles is still not clear without the understanding of the soil dynamics, the radiocarbon provides a simple and convenient method to study the turnover of the soil organic matter (SOM). Several models and methods in the study of soil organic matter turnover by the application of radiocarbon were introduced in this paper. It was pointed out that the SOM radiocarbon application may be used to study the carbon cycle of longer time scale such as decades and more, whereas its application to the soil CO2 can be used to study the carbon cycle of shorter time scale such as seasons or one year. Other applications such as those in the study of fine root age and land use change were also introduced in this paper. Although radiocarbon had been used in the study of carbon cycle, its application was very limited so far and some problems had been found. At last, some issues unsettled were put forward and the future development direction and fields using this method to study the SOM dynamics were introduced.

Cite this article

WANG Lin, OUYANG Hua, ZHOU Caiping, SONG Minghua, TIAN Yuqiang, . The Application of Radiocarbon in the Study of Soil Carbon Cycles[J]. PROGRESS IN GEOGRAPHY, 2004 , 23(4) : 43 -51 . DOI: 10.11820/dlkxjz.2004.04.006

References


[1] Schlesinger W H. Evidence from chronosequence studies for a low carbon-storage potential of soil. Nature. 1990, 348: 232~234.

[2] Wang Y, Amundson R. The impact of land use change on C turnover in soils. Global Biogeochemical Cycles. 1999, 13 (1): 47~57.

[3] Oades J M. The retention of organic matter in soils. Biogeochemistry. 1994, 5: 35~70.

[4] Schimel D S. Terrestrial ecosystems and the carbon cycle. Global Change Biology. 1995, 1: 77~91.

[5] 陈庆强, 沈承德, 易惟熙等. 土壤碳循环研究进展. 地球科学进展. 1998,13(6):555~563.

[6] Torn M S, Trumbore S E, Chardwick O A, et al. Mineral control of soil organic carbon storage and turnover. Nature. 1997, 389: 170~173.

[7] Trumbore S E. Comparison of carbon dynamics in tropical and temperate soils using radiocarbon measurements. Global Biogeochemical Cycles. 1993, 7(2): 275~290.

[8] Balesdent J. The turnover of soil organic fractions estimated by radiocarbon dating. Sci Total Environ. 1987, 62: 405~408.

[9] Trumbore S E, Vogel J S, Southon J R. AMS 14C measurements of fractionated soil organic matter: an approach to deciphering the soil carbon cycle. Radiocarbon. 1989, 31: 644~654.

[10] Wang Y, Hsieh Y P. Uncertainties and novel prospects in the study of the soil carbon dynamics. Chemosphere. 2002, 49: 791~804.

[11] Arnold, J R, Libby W F. Age determinations by radiocarbon content: Checks with samples of known age. Science. 1949, 110: 678~680.

[12] Stuiver M, Polach H. Reporting of 14C data. Radiocarbon. 1977, 17: 355~363.

[13] Donahue D, Linick T, Tull J. Isotope-ratio and background corrections for accelerator mass spectrometry radiocarbon measurements. Radiocarbon. 1990, 32: 135~142.

[14] Trumbore S E, Chadwick O A, Amundson R. Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change. Science. 1996, 272: 393~396.

[15] Jenkinson D S, Harkness D D, Vance E D, et al. Calculating net primary production and annual input of organic matter to soil from the amount and radiocarbon content of soil organic matter. Soil Biology and Biochemistry. 1990, 24: 295~308.

[16] Harrison K, Broecker W, Bonani G. The effect of changing land use on soil radiocarbon. Science. 1993, 262: 725~726.

[17] Hsieh Y P. Radiocarbon signatures of turnover rates in active soil organic carbon pools. Soil Science Society of America Journal. 1993, 57: 1020~1022.

[18] Wang Y, Amundson R, Trumbore S E. Radiocarbon dating of soil organic matter. Quaternary Research. 1996, 45: 282~288.

[19] Neff J C, Townsend A R, Gleixner G, et al. Variable effects of nitrogen additions on the stability and turnover of soil carbon. Nature. 2002, 419: 915~917.

[20] Trumbore S E, Harden J W. Accumulation and turnover of carbon in organic and mineral soils of the BOREAS northern study area. Journal of Geophysical Research. 1997, 102 ( D24): 28817~28830.

[21] Cherkinsky A E, Brovkin V A. Dynamics of radiocarbon in soils. Radiocarbon. 1993, 35 (3): 363~367.

[22] Burchuladze A A, Chudy M, Eristave I V, et al. Anthropogenic 14C variations in atmospheric CO2 and wines. Radiocarbon. 1989, 31: 771~776.

[23] Levin I, Kromer B. Twenty years of atmospheric (CO2)-C-14 observations at Schauinsland station,Germany. Radiocarbon. 1997, 39: 205~218.

[24] Levin I, Hesshaimer V. Radiocarbon-a unique tracer of the global carbon cycle dynamics. Radiocarbon. 2000, 42: 69~80.

[25] Suess H E. Radiocarbon content in modern wood. Science. 1955, 122: 415~417.

[26] Chen Q Q, Sun Y M, Shen C D, et al. Organic matter turnover rates and CO2 flux from organic matter decomposition of mountain soil profiles in the subtropical area, south China. Catena. 2002, 49: 217~229.

[27] Wang Y, Amundson R, Niu X F. Seasonal and altitudinal variation in decomposition of soil organic matter inferred from radiocarbon measurements of soil CO2 flux. Global Biogeochemical Cycles. 2000, 14: 199~211.

[28] Hasson P J, Edwards N T, Garten C T, et al. Separating root and soil microbial contributions to soil respiration: a review of methods and observations. Biogeochemistry. 2000, 48: 115~146.

[29] Post W, Izaurralde R, Mann L, et al. Monitoring and verifying soil organic carbon sequestration. In: Rosenberg N, Izaurralde R, Malone E. Carbon sequestration in soils—Science, Monitoring, and Beyond. Proceedings of the St. Michaels Workshop. Columbus: Battelle Press. 1998, 41~66.

[30] Trumbore S E. Age of soil organic matter and soil respiration: Radiocarbon constraints on belowground C dynamics. Ecological Applications. 2000, 10: 399~411.

[31] John B, Pandey H N, Tripathi R S. Vertical distribution and seasonal changes of fine and coarse root mass in Pinus kesiya Royle Ex.Gordon forest of three different ages. Acta Oecologica. 2001,22: 293~300.

[32] Jackson R B, Mooney H A, Schulze E D. A global budget for fine root biomass, surface area, and nutrient contents. Proc. Natl. Acad. Sci. USA. 1997, 94: 7362~7366.

[33] Fahey T J, Hughes J W. Fine root dynamics in a northern hardwood forest ecosystem, Hubbard Brook Experimental Forest, NH. Journal of Ecology. 1994, 82: 533~548.

[34] Vogt K A, Vogt D J, Bloomfield J. Analysis of some direct and indirect methods for estimating root biomass and production of forests at an ecosystem level. Plant Soil. 1998, 200: 71~89.

[35] Aber J D, Melillo J M, Nadelhoffer K J, et al. Fine root turnover in forest ecosystems in relation to quantity and form of nitrogen availability: a comparison of two methods. Oecologia. 1985, 66: 317~321.

[36] Gaudinski J B, Trumbore S E, Davidson E A, et al. The age of fine-root carbon in three forests of the eastern United States measured by radiocarbon. Oecologia. 2001, 129: 420~429.

[37] Tierney G L, Fahey T J. Fine root turnover in a northern hardwood forest: a direct comparison of the radiocarbon and minirhizotron methods. Canadian Journal of Forest Research. 2002, 32: 1692~1697.

[38] Richter D D, Markewitz D, Trumbore S E, et al. Rapid accumulation and turnover of soil carbon in a re-establishing forest. Nature. 1999,400: 56~58.

[39] Perrin R M S, Willis E H, Hodge, D A H. Dating of humus podzols by residual radiocarbon activity. Nature. 1964, 202: 165~166.

[40] Scharpenseel H W, Becher H P. 25 years of radiocarbon dating soils: a paradigm of erring and learning. Radiocarbon. 1991, 33: 238.

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