Concurrent changes in soil inorganic and organic carbon during the development of larch, Larix gmelinii, plantations and their effects on soil physicochemical properties
详细信息 查看全文
- 作者：Wenjie Wang (1)
Dongxue Su (1)
Ling Qiu (1)
Hongyan Wang (1)
Jing An (1)
Guangyu Zheng (1)
Yuangang Zu (1) - 关键词：Soil inorganic carbon (SIC) ; Soil organic carbon (SOC) ; Soil physicochemical properties ; Larix gmelinii plantation
- 刊名：Environmental Earth Sciences
- 出版年：2013
- 出版时间：July 2013
- 年：2013
- 卷：69
- 期：5
- 页码：1559-1570
- 全文大小：579KB
- 参考文献：1. Bao SD (2000) Soil and agricultural chemistry analysis, 3rd edn. China Agriculture Press, Beijing
2. Bronick CJ, Lal R (2005) Soil structure and management: a review. Geoderma 124:3-2 CrossRef
3. Chen LX, Xiao Y (2006) Evolution and evaluation of soil fertility in forest land in / Larix gmelinii plantations at different development stages in Daxinganling forest region. Sci Soil Water Conserv 5:50-5
4. Covington W (1981) Changes in forest floor organic matter and nutrient content following clear cutting in northern hardwoods. Ecology 62:41-8 CrossRef
5. Duan JN, Li BG, Shi YC, Yan TL, Zhu DH (1999) Modeling of soil CaCO3 deposition process in arid areas. Acta Pedol Sin 36:318-26
6. Enoki T, Kawaguchi H, Iwatsubo G (1996) Topographic variations of soil properties and stand structure in a Pinus thunbergii plantation. Ecol Res 11:299-09 CrossRef
7. Entry JA, Sojka RE, Shewmaker GE (2004) Irrigation increases inorganic carbon in 550 agricultural soils. Environ Manage 33:309-17
8. Eswaran H, Van den Berg E, Reich P, Kimble J (1995) Global soil carbon resources. In: Lal R, Kimble J, Levine E, Stewart BA (eds) Soil and global change. CRC/Lewis Publishers, Boca Raton, pp 27-3
9. Garten CT (2002) Soil carbon storage beneath recently established tree plantations in Tennessee and South Carolina, USA. Biomass Bioenergy 23:93-02 CrossRef
10. Garten Jr, Huston MA, Thoms CA (1994) Topographic variation of soil nitrogen dynamics at Walker Branch watershed, Tennessee. For Sci 40:497-12
11. Gleixner GD, Tefs C, Jordan A et al (2009) Soil carbon accumulation in old-growth forests. In: Wirth C, Gleixner G, Heimann M (eds) Old-growth forests: function, fate and value. Springe, Berlin, pp 231-66 CrossRef
12. Goh TB, Arnaud RJ, Mermut AR (1993) Carbonates. In: Carter MR (ed) Soil sampling and methods of analysis. Lewis Publishers, Boca Raton, pp 177-85
13. Han YZ, Liang SF (1997) A research on root distribution and biomass of North-China larch. Shanxi For Sci Tech 3:36-0
14. Hansen EA (1993) Soil carbon sequestration beneath hybrid poplar plantations in the 565 North Central United States. Biomass Bioenergy 5:431-36 CrossRef
15. HLJTR (1992) Soil of Heilongjiang Province. Science and Technology press of Heilongjiang Province, Harbin
16. Kajimoto T, Osawa A, Matsuura Y, Abaimov AP, Zyryanova OA, Kondo K, Tokuchi N, Hirobe M (2007) Individual-based measurement and analysis of root system development: case studies for / Larix gmelinii trees growing on the permafrost region in Siberia. J For Res 12:103-12 CrossRef
17. Klopatek JM (2002) Below ground carbon pools and processes in different age 570 stands of Douglas-fir. Tree Physiol 22:197-04 CrossRef
18. Kravchenko AN, Robertson GP (2011) Whole-profile soil carbon stocks: the danger of assuming too much from analyses of too little. Soil Sci Soc Am J 75:235-40 CrossRef
19. Lal R (2002) Soil carbon sequestration in china through agricultural intensification, and restoration of degraded and desertified ecosystems. Land Degrad Dev 13:469-78 CrossRef
20. Lal R (2004) Soil carbon sequestration impacts on global climate change and food 580 security. Science 304:1623-627 CrossRef
21. Lal R, Kimble JM (2000) Pedogenic carbonates and the global carbon cycle: global 575 climate change and pedogenic carbonates. CRC Press, Boca Raton
22. Law BE, Sun OJ, Campbell J, Van Tuyl S, Thornton PE (2003) Changes in carbon storage and fluxes in a chronosequence of ponderosa pine. Glob Change Biol 9:510-24 CrossRef
23. Li XY, Li BG, Lu HY (1999) Modeling and simulation of dynamic carbonate deposition in a loess-paleosol sequence. Chin Sci Bull 44:211-17
24. Li ZP, Han FX, Su Y, Zhang TL, Sun B, Monts DL, Plodine MJ (2007) Assessment of soil organic and carbonate carbon storage in China. Geoderma 138:119-26 CrossRef
25. Liu SR, Wang WZ, Wang MQ (1992) The characteristics of energy in the formative process of net primary productivity of larch artificial forest ecosystem. Acta Phytoecologica et Geobotanica Sinica 16:209-19
26. Lorenz K, Lal R, Shipitalo MJ (2011) Stabilized soil organic carbon pools in subsoils under forest are potential sinks for atmospheric CO2. For Sci 57:19-5
27. Lu XJ, Gao H, Xu SW, Zheng KX (1999) Studies on the influences of continuous 595 planting of larch on soil physical properties and tree growth. J Liaoning For Sci Technol 5:10-2
28. Luo YJ, Zhang XQ, Hou ZH, Yu PT, Zhu JH (2007) Biomass carbon accounting factors of Larix forests in china based on literature data. J Plant Ecol 6:1111-118
29. Luyssaert SE, Schulze ED, B?rner A, Knohl A, Hessenm?ller D, Law BE, Ciais P, Grace J (2008) Old-growth forests as global carbon sinks. Nature 455:213-15 CrossRef
30. Ming DW (2002) Carbonates. Encyclopedia of Soil Science, New York
31. NEFU (1984) Basic data for Maoershan experimental Forest farm of northeast Forestry University. NEFU press, Harbin
32. Pan GX (1999) Pedogenic carbonates in aridic soils of China and the significance in terrestrial carbon transfer. J Nanjing Agric Univ 20:325-34
33. Post WM, Emanuel WR, Zinke PJ, Stangenberger AG (1982) Soil carbon pools and world life zones. Nature 298:156-59 CrossRef
34. Richter DD, Markewitz D, Trumbore SE, Wells CG (1999) Rapid accumulation and turnover of soil carbon in a re-establishing forest. Nature 400:56-8 CrossRef
35. Sartori F, Lal R, Ebinger MH, Eaton JA (2007) Changes in soil carbon a610 nd nutrient pools along a chronosequence of poplar plantations in the Columbia Plateau, Oregon, USA. Agric Ecosyst Environ 122:325-39 CrossRef
36. Schedlbauer JL, Kavanagh KL (2008) Soil carbon dynamics in a chronosequence of secondary forests in northeastern Costa Rica. For Ecol Manage 255:1326-335 CrossRef
37. Schlesinger WH (2002) Inorganic carbon and the global carbon cycle., Encyclopedia of soil scienceMarcel Dekker, New York
38. Serrano-Ortiz P, Roland M, Sanchez-Moral S, Janssens IA, Domingo F, Godderis Y, Kowalski AS (2010) Hidden, abiotic CO2 flows and gaseous reservoirs in the terrestrial carbon cycle: review and perspectives. Agric For Meteorol 150:321-29 CrossRef
39. Singh SK, Singh AK, Sharma BK, Tarafdar JC (2007) Carbon stock and organic carbon dynamics in soils of Rajasthan, India. J Arid Environ 68:408-21 CrossRef
40. Springsteen A, Loya W, Liebig M, Hendrickson J (2010) Soil carbon and nitrogen across a chronosequence of woody plant expansion in North Dakota. Plant Soil 328:369-79 CrossRef
41. Sun YJ, Zhang J, Han AH, Wang XJ (2007) Biomass and carbon pool of / Larix gmelinii young and middle age forest in Xing’an Mountains Inner Mongolia. Acta Ecol Sin 27:1756-762
42. Walker LR, Wardle DA, Bardgett RD, Clarkson BD (2010) The use of chronosequences in studies of ecological succession and soil development. J Ecol 98:725-36 CrossRef
43. Wang Z (1992) Larix forests in China. China Forestry Press, Beijing
44. Wang WJ, Zu YG, Wang HM, Matsuura Y, Sasa K, Koike T (2005a) Plant biomass and productivity of / Larix gmelinii forest ecosystems in Northeast China: intra-and inter-species comparison. Eurasian J Res 8:21-1
45. Wang WJ, Zu YG, Wang HM, Hirano T, Sasa K, Koike T (2005b) Effect of collar 640 insertion on soil respiration in a larch forest measured with a LI-6400 soil CO2 flux system. J For Res 10:57-0 CrossRef
46. Wang WJ, Qiu L, Zu YG, Su DX, An J, Wang HY, Zheng GY, Sun W, Chen XQ (2011) Changes in soil organic carbon, nitrogen, pH and bulk density with the development of larch plantations in China. Glob Change Biol 17:2657-676 CrossRef
47. Wen QZ (1989) Loess geochemistry in China. Science Press, Beijing
48. Wirth C, Czimczik CJ, Schulze ED (2002) Beyond annual budgets: carbon flux a650 t different temporal scales in fire-pron Siberian Scots pine forests. Tellus Ser B Chem Phys Meteorol 54:611-30 CrossRef
49. Wu H, Guo Z, Gao Q, Peng C (2009) Distribution of soil inorganic carbon storage and its changes due to agricultural land use activity in China. Agric Ecosyst Environ 129:413-21 CrossRef
50. Zhou GY, Liu SG, Li Z, Zhang DQ, Tang XL, Zhou CY, Yan JH, Mo J (2006) Old-growth forests can accumulate carbon in soils. Science 314:1417 CrossRef
51. Zu YG, Li R, Wang WJ, Su DX, Wang Y, Qiu L (2011) Soil organic and inorganic carbon contents in relation to soil physicochemical properties in northeastern China. Acta Ecologica Sinica 31:5207-216 - 作者单位：Wenjie Wang (1)
Dongxue Su (1)
Ling Qiu (1)
Hongyan Wang (1)
Jing An (1)
Guangyu Zheng (1)
Yuangang Zu (1)
1. Key Laboratory of Forest Plant Ecology, Northeast Forestry University, Harbin, 150040, People’s Republic of China - ISSN：1866-6299
文摘
Soil inorganic carbon (SIC) and organic carbon (SOC) levels can change with forest development, however, concurrent changes in soil carbon balance and their functional differences in regulating soil properties are unclear. Here, SIC, SOC, and other physicochemical properties of soil (N, alkali-hydrolyzed N, effective Si, electrical conductivity, pH, and bulk density) in 49 chronosequence plots of larch plantation forests were evaluated, by analyzing the concurrent changes in SIC and SOC storage during growth of plantation and the functional difference of these levels in maintaining soil sustainability. These soils had characteristically high SOC (15.34?kg?m?) and low SIC storage (83.38?g?m? on average). Further, 28 of 30 linear regressions between SIC and SOC storage and larch growth parameters (age, tree size, and biomass density) were not statistically significant (p?>?0.05). However, significant changes were observed in ratios of SIC and SOC with these growth parameters (between 0-0?cm and 40-0?cm, respectively; p?<?0.05). These results were more useful for determining the changes in SIC and SOC vertical distribution than changes in storage. Moreover, larch growth generally decreased SIC and increased SOC. Linear correlation and multiple-regression analysis showed that the SIC influences soil acidity, whereas SOC affects soil nitrogen. This clearly indicates that larch growth could result in divergent changes in SIC and SOC levels, particularly in their vertical distribution; further, changes in SIC and SOC may variably affect soil physicochemical properties.