[an error occurred while processing this directive] [an error occurred while processing this directive]
[an error occurred while processing this directive]红壤侵蚀区芒萁对土壤可溶性有机质光谱特征的影响
网络出版日期: 2017-09-29
基金资助
国家自然科学基金(31370465)和国家重点基础研究发展计划(973计划)前期专项课题(2012CB722203)。
Effect of Dicranopteris dichotoma on spectroscopic characteristic of dissolved organic matter in red soil erosion area
Online published: 2017-09-29
可溶性有机质(DOM)是森林生态系统能量循环的主要载体, 在碳循环过程中发挥着重要的作用。为了深入了解植被恢复后土壤DOM的变化和结构特征, 在典型红壤侵蚀区福建省龙岩市长汀县河田镇选取不同恢复年限的马尾松(Pinus massoniana)林为研究对象, 利用光学技术对比分析了不同恢复年限(0年, 13年, 31年)马尾松林保留芒萁(Dicranopteris dichotoma)覆盖地、去除芒萁覆盖地和林下裸地土壤DOM光谱特征。结果表明: 未治理地(Y0)、恢复13年(Y13)和恢复31年(Y31)马尾松林芒萁覆盖地土壤可溶性有机碳(DOC)含量分别是林下裸地的7.61倍、4.83倍和5.47倍, 去除芒萁一年后, 土壤DOC的含量显著下降, 但仍分别是林下裸地的1.84倍、4.12倍和4.73倍; 芒萁覆盖地土壤DOM的芳香化指数(AI)和腐殖化指数(HIX)均显著高于林下裸地, 而波长在250 nm和365 nm处的紫外可见光光度值之比(E2:E3)的趋势与之相反, 去除芒萁一年后, AI和HIX降低显著, 表明芒萁覆盖地土壤DOM腐殖化和芳香化程度更高, 分子量更大; 林下裸地DOM红外光谱中特征峰明显不如林下芒萁覆盖地丰富, 其含有更多的羟基、羧酸类, 以及碳水化合物中的烷氧基等结构简单、易迁移的物质, 去除芒萁一年后, DOM红外光谱特征峰无明显变化, 表明芒萁是土壤DOM数量和结构的主要影响因素, 而这种影响是一个长期缓慢的过程。从DOM光谱分析结果可知, 芒萁覆盖下土壤DOM的分子量更大, 结构更复杂, 易于被土壤胶粒吸附, 维持其化学稳定, 利于土壤有机碳积累。由此可见, 芒萁在土壤有机碳积累过程中具有积极的作用。
张浩, 吕茂奎, 谢锦升 . 红壤侵蚀区芒萁对土壤可溶性有机质光谱特征的影响[J]. 植物生态学报, 2017 , 41(8) : 862 -871 . DOI: 10.17521/cjpe.2016.0363
Aims Dissolved organic matter (DOM) is the most active component of organic matters in soils, and plays an important role in carbon cycles. It is a mixed organic compound with varying molecular sizes and weights. We aimed to explore the impacts of Dicranopteris dichotoma coverage on quantity and structure of DOM after vegetation restoration in severely eroded red soil region. Methods A typical sequence of vegetation restoration (Y0, without ecological restoration; Y13, ecological restoration for 13 years; Y31, ecological restoration for 31 years) was selected as the research object in Hetian Town, Changting County, Fujian Province, China. At each experimental site, soils were subject to three treatments—NRd, not removed D. dichotoma; Rd, removed D. dichotoma; and CK, control, and the effects of D. dichotoma on the spectral characteristics of DOM were evaluated.Important findings The results indicated that the quantity of soil DOC under NRd treatment of the Y0, Y13 and Y31 was 7.61, 4.83, and 5.47 times higher than their CK treatment, respectively. The Rd treatment had significantly lower DOC than that under NRd treatments, and it was 1.84, 4.12, and 4.73 times higher than their CK treatments, respectively. Thus the D. dichotoma had exerted significant effects on the quantity of soil DOM. The Aromaticity index (AI), emission fluorescence spectrum humification index (HIXem) and synchronous fluorescence spectrum humification index (HIXsyn) of DOM under the NRd treatment were significantly higher than those of the CK treatments in Y13 and Y31, respectively. However, the ratio of ultraviolet-visible light absorption photometric quantity at 250 nm wavelength to ultraviolet-visible light absorption photometric quantity at 365 nm wavelength (E2:E3) had an opposite trend. It showed that the DOM structure in soils covered by D. dichotoma contained more aromatic nucleus and had higher aromaticity and humification, and DOM molecular was larger. In addition, the AI and humification index (HIX) of DOM under the Rd treatment was significantly decreased compared with the NRd treatment. Similar results were observed by analysis of emission and synchronous fluorescence spectrum, and by the Fourier infrared transmission spectrum analysis. These results suggest that D. dichotoma had positive impacts on the complexity of DOM structure, but it was a long and slow process. The DOM spectral analysis showed that the soil DOM covered by D. dichotoma had a stable and complex structure and was easily adsorbed by soil colloid. As a result, Dicranopteris dichotoma had a positive effect on the accumulation of soil organic carbon.
[1] | Akagi J, ádám Zsolnay, Bastida F (2007). Quantity and spectroscopic properties of soil dissolved organic matter (DOM) as a function of soil sample treatments: Air-drying and pre-incubation.Chemosphere, 69, 1040-1046. |
[2] | Andreasson F, Bo B, B??th E (2009). Bioavailability of DOC in leachates, soil matrix solutions and soil water extracts from beech forest floors.Soil Biology & Biochemistry, 41, 1652-1658. |
[3] | Carter HT, Tipping E, Koprivnjak JF, Millerc PM, Cooksond B, Hamilton-Taylord J (2012). Freshwater DOM quantity and quality from a two-component model of UV absorbance.Water Research, 46, 4532-4542. |
[4] | Chang SC, Wang CP, Feng CM, Rees R, Hell U, Matzner E (2007). Soil fluxes of mineral elements and dissolved organic matter following manipulation of leaf litter input in a Taiwan Chamaecyparis forest.Forest Ecology & Management, 242, 133-141. |
[5] | Fujii K, Uemura M, Hayakawa C, Funakawa S (2009). Fluxes of dissolved organic carbon in two tropical forest ecosystems of East Kalimantan, Indonesia. Geoderma, 152, 127-136. |
[6] | Gielen B, Neirynck J, Luyssaert S, Janssens IA (2011). The importance of dissolved organic carbon fluxes for the carbon balance of a temperate Scots pine forest.Agricultural and Forest Meteorology, 151, 270-278. |
[7] | Hagedorn F, Kaiser K, Feyen H, Schleppi P (2000). Effects of redox conditions and flow processes on the mobility of dissolved organic carbon and nitrogen in a forest soil.Journal of Environmental Quality, 29, 288-297. |
[8] | Jiao K, Li ZP (2005). Dynamics and biodegradation of dissolved organic carbon in paddy soils derived from red clay. Soils, 37, 272-276.(in Chinese with English abstract)[焦坤, 李忠佩 (2005). 红壤稻田土壤溶解有机碳含量动态及其生物降解特征. 土壤,37, 272-276.] |
[9] | Kaiser K (1997). Dissolved organic matter sorption on subsoil and minerals studied by 13C-NMR and DRIFT spectroscopy.European Journal of Soil Science, 48, 301-310. |
[10] | Kalbitz K, Geyer W, Geyer S (1999). Spectroscopic properties of dissolved humic substances—A reflection of land use history in a fen area.Biogeochemistry, 47, 219-238. |
[11] | Kalbitz K, Kaiser K (2008). Contribution of dissolved organic matter to carbon storage in forest mineral soils.Journal of Plant Nutrition & Soil Science, 171, 52-60. |
[12] | Kalbitz K, Meyer A, Yang R, Gerstberger P (2007). Response of dissolved organic matter in the forest floor to long-term manipulation of litter and throughfall inputs.Biogeochemistry, 86, 301-318. |
[13] | Li HT, Yu GR, Li JY, Chen YR, Liang T (2007). Decomposition dynamics and nutrient release of litters for four artificial forests in the red soil and hilly region of subtropical China.Acta Ecologica Sinica, 27, 898-908.(in Chinese with English abstract)[李海涛, 于贵瑞, 李家永, 陈永瑞, 梁涛 (2007). 亚热带红壤丘陵区四种人工林凋落物分解动态及养分释放. 生态学报,27, 898-908.] |
[14] | Liu Z, Yang YS, Zhu JM, Xie JS, Si YT (2015). Effects of forest conversion on quantities and spectroscopic characteristics of soil dissolved organic matter in subtropical China.Acta Ecologica Sinica, 35, 6288-6297.(in Chinese with English abstract) [刘翥, 杨玉盛, 朱锦懋, 谢锦升, 司友涛 (2015). 中亚热带森林转换对土壤可溶性有机质数量与光谱学特征的影响. 生态学报,35, 6288-6297.] |
[15] | Mccarthy JF (2005). Carbon fluxes in soil.Journal of Geographical Sciences, 15, 149-154. |
[16] | Michalzik B, Matzner E (1999). Dynamics of dissolved organic nitrogen and carbon in a Central European Norway spruce ecosystem.European Journal of Soil Science, 50, 579-590. |
[17] | Peuravuori J, Pihlaja K (1997). Molecular size distribution and spectroscopic properties of aquatic humic substances.Analytica Chimica Acta, 337, 133-149. |
[18] | Schwendenmann L, Veldkamp E (2005). The role of dissolved organic carbon, dissolved organic nitrogen, and dissolved inorganic nitrogen in a tropical wet forest ecosystems.Ecosystems, 8, 339-351. |
[19] | Wu JS, Jiang PK, Chang SX, Xu QF, Lin Y (2010). Dissolved soil organic carbon and nitrogen were affected by conversion of native forests to plantations in subtropical China. Canadian Journal of Soil Science, 90, 27-36. |
[20] | Xiao YC, Dou S (2008). Study on infrared spectra of soil humus fractions.Chinese Journal of Analytical Chemistry, 35, 1596-1600.(in Chinese with English abstract) [肖彦春, 窦森 (2008). 土壤腐殖质各组分红外光谱研究. 分析化学,35, 1596-1600.] |
[21] | Xie JS, Guo JF, Yang ZJ, Huang ZQ, Chen GS, Yang YS (2013). Rapid accumulation of carbon on severely eroded red soils through afforestation in subtropical China. Forest Ecology & Management, 300, 53-59. |
[22] | Yang YS, Guo JF, Chen GS, Chen YX, Yu ZY, Liu DX (2003). Origin, property and flux of dissolved organic matter in forest ecosystems.Acta Ecologica Sinica, 23, 547-558.(in Chinese with English abstract)[杨玉盛, 郭剑芬, 陈光水, 陈银秀, 于占源, 董彬, 刘东霞 (2003). 森林生态系统DOM的来源、特性及流动. 生态学报,23, 547-558.] |
[23] | Zhan XH, Zhou LX, Yang H, Jiang TH (2007). Infrared spectroscopy of DOM-PAHs complexes.Acta Pedologica Sinic, 44, 47-53.(in Chinese with English abstract)[占新华, 周立祥, 杨红, 蒋廷惠 (2007). 水溶性有机物与多环芳烃结合特征的红外光谱学研究. 土壤学报,44, 47-53.] |
[24] | Zhang H, Lyu MK, Jiang J, Pu XT, Wang EX, Qiu X, Xie JS (2016). Effect of vegetation restoration on topsoil and subsoil organic carbon mineralization in red soil erosion area,Journal of Soil and Water Conservation, 30, 244-249.(in Chinese with English abstract)[张浩, 吕茂奎, 江军, 蒲晓婷, 王恩熙, 邱曦, 谢锦升 (2016). 侵蚀红壤区植被恢复对表层与深层土壤有机碳矿化的影响. 水土保持学报,44, 244-249.] |
[25] | Zhao J, Wan S, Li Z, Shao Y, Xu G, Liu Z, Zhou L, Fu S (2012). Dicranopteris-dominated understory as major driver of intensive forest ecosystem in humid subtropical and tropical region.Soil Biology & Biochemistry, 49, 78-87. |
[26] | Zhou GM, Jiang PK (2004). Changes in active organic carbon of erosion red soil by vegetation recovery. Journal of Soil and Water Conservation, 18, 68-70.(in Chinese with English abstract)[周国模, 姜培坤 (2004). 不同植被恢复对侵蚀型红壤活性碳库的影响. 水土保持学报,18, 68-70.] |
[27] | Zhou JM, Dai JY, Pan GX (2004). Fractionation and spectroscopic property of dissolved organic matters in soils.Spectroscopy and Spectral Analysis, 24, 1060-1065.(in Chinese with English abstract)[周江敏, 代静玉, 潘根兴 (2004). 应用光谱分析技术研究土壤水溶性有机质的分组及其结构特征. 光谱学与光谱分析,24, 1060-1065.] |
[28] | Zhu HJ (1992). Soil Geography. Higher Education Press, Beijing.(in Chinese)[朱鹤健 (1992). 土壤地理学. 高等教育出版社, 北京.] |
/
〈 |
|
〉 |