石漠化山区森林植被退化与水源涵养服务的关系研究进展
Research Progress on the Relationship between Forest Vegetation Degradation and Water Conservation Service in Rocky Desertification Mountain Area
DOI: 10.12677/WJF.2020.92007, PDF,    科研立项经费支持
作者: 李昌兰*:贵阳市花溪区黔陶乡生态保护站,贵阳 贵州
关键词: 水源涵养服务植被退化研究进展石漠化山区Water Conservation Services Vegetation Degradation Research Progress Rocky Desertification Mountain Area
摘要: 石漠化是中国西南地区最严重的生态环境问题,石漠化区森林植被退化与服务其生长的水源情况关系密切,历来受到科研工作者的广泛关注。本文采用文献分析法,分析了石漠化山区植被退化特征、水源涵养服务功能及其二者关系的研究现状及发展动态,目前在退化植被结构及功能、枯落物和土壤水分运移规律及异质性等方面进行大量研究,部分研究也揭示了植物水分利用来源,但未能揭示水源涵养服务在喀斯特植被退化过程中的作用与机理。今后应从枯落物层、土壤层及岩溶裂隙水分的角度去阐明喀斯特退化生态系统水源涵养服务的提供,同时针对水分是石漠化区主要限制性生态因子,从水源涵养功能变化及其服务去认识石漠化山区植被退化过程。
Abstract: Rocky desertification is the most serious ecological and environmental problem in Southwest China. The degradation of forest vegetation in the rocky desertification is closely related to the water supply that serves its growth, which has always been widely concerned by researchers. By using the method of literature analysis, this paper analyzes the research status and development trends of vegetation degradation characteristics, water conservation service function and their relationship in rocky desertification mountainous areas. At present, a lot of researches have been carried out in the structure and function of degraded vegetations, the movement and heterogeneity of water in litter and soil. Some researchers also have revealed the source of plant water use, but they fail to reveal the role and mechanism of water conservation services in the process of karst vegetation degradation. In future, more attentions should be paid to the provision of water conservation services for karst degraded ecosystem. Water is the main limiting ecological factor in rocky desertification area. Moreover, it should be considered that the process of vegetation degradation in rocky desertification mountain area should be understood from the change of water conservation function and its services.
文章引用:李昌兰. 石漠化山区森林植被退化与水源涵养服务的关系研究进展[J]. 林业世界, 2020, 9(2): 49-55. https://doi.org/10.12677/WJF.2020.92007

参考文献

[1] 杨瑞, 喻理飞. 退化喀斯特森林自然恢复过程中的冠层结构特征及其动态变化[J]. 中国水土保持科学, 2015(4): 36-40.
[2] 喻理飞, 朱守谦, 叶镜中, 等. 退化喀斯特森林自然恢复过程中群落动态研究[J]. 林业科学, 2002, 38(1): 1-7.
[3] 吴毅, 刘文耀, 沈有信. 云南石林景区主要乡土植物物候特征的初步研究[J]. 山地学报, 2006, 24(6): 647-653.
[4] 曹建华, 袁道先, 章程, 等. 受地质条件制约的中国西南岩溶生态系统[J]. 地球与环境, 2004, 32(1): 1-8.
[5] 邓艳, 蒋忠诚, 曹建华. 弄拉典型峰丛岩溶区青冈栎叶片形态特征及对环境的适应[J]. 广西植物, 2004, 24(4): 317-322.
[6] 俞月凤, 何铁光, 杜虎, 等. 桂西北喀斯特地区不同退化程度植被群落物种组成及多样性特征[J]. 广西植物, 2019(2): 178-188.
[7] 朱守谦. 贵州喀斯特地区植被恢复的理论与实践[J]. 贵州环境科学, 2000(1): 31-41.
[8] 李先琨, 蒋忠诚, 黄玉清, 等. 桂西南岩溶山地优势植物种群动态及其对岩溶作用的影响[J]. 地球学报, 2008, 29(2): 253-259.
[9] 张平, 蔡光丽, 沈有信, 等. 滇东南岩溶山地退化植被土壤种子库的储量与组成[J]. 植物生态学报, 2004, 28(1): 101-106.
[10] 李阳兵, 魏朝富, 李先源, 等. 土地利用方式对岩溶山地土壤种子库的影响[J]. 山地学报, 2002, 20(3): 319-324.
[11] 欧阳绪红, 郝秀东, 谢世友, 等. 喀斯特山地典型植被恢复过程中土壤种子库特征[J]. 湖北农业科学, 2011, 50(15): 3049-3053.
[12] 张笑楠, 王克林, 陈洪松, 等. 桂西北喀斯特区域景观结构特征与石漠化的关系[J]. 应用生态学报, 2008(11): 143-148.
[13] Mol, G. and Keesstra, S. (2012) Soil Science in a Changing World. Current Opinion in Environmental Sustainability, 4, 473-477. [Google Scholar] [CrossRef
[14] Keesstra, S.D., Bouma, J., Wallinga, J., et al. (2016) The Significance of Soils and Soil Science towards Realization of the United Nations Sustainable Development Goals. Soil, 2, 111-128. [Google Scholar] [CrossRef
[15] Peng, X., Shi, D., Guo, H., et al. (2015) Effect of Urbanisation on the Water Retention Function in the Three Gorges Reservoir Area, China. Catena, 133, 241-249. [Google Scholar] [CrossRef
[16] Shi, D., Wang, W., Jiang, G., et al. (2016) Effects of Disturbed Landforms on the Soil Water Retention Function during Urbanization Process in the Three Gorges Reservoir Region, China. Catena, 144, 84-93. [Google Scholar] [CrossRef
[17] Parchami-Araghi, F., Mirlatifi, S.M., Dashtaki, S.G., et al. (2013) Point Estimation of Soil Water Infiltration Process Using Artificial Neural Networks for Some Calcareous Soils. Journal of Hydrology, 481, 35-47. [Google Scholar] [CrossRef
[18] Mao, L.L., Li, Y.Z., Hao, W.P., et al. (2016) An Approximate Point Source Method for Soil Infiltration Process Measurement. Geoderma, 264, 10-16. [Google Scholar] [CrossRef
[19] 张志才, 陈喜, 石朋, 等. 岩石对喀斯特峰丛山体土壤水分布特征的影响[J]. 水土保持通报, 2008(6): 45-48.
[20] 蒋光毅, 黄先智, 史东梅, 等. 石漠化区桑树地埂的土壤水分特征研究[J]. 水土保持学报, 2015, 29(6): 217-223.
[21] 张继光, 陈洪松, 苏以荣, 等. 喀斯特山区坡面土壤水分变异特征及其与环境因子的关系[J]. 农业工程学报, 2010, 26(9): 87-93.
[22] 刘海隆, 蒋太明, 刘洪斌, 等. 不同土地利用方式对岩溶山区旱坡地土壤水分时空分异的影响[J]. 土壤学报, 2005, 42(3): 428-433.
[23] 李孝良, 陈效民, 周炼川, 等. 西南喀斯特石漠化过程对土壤水分特性的影响[J]. 水土保持学报, 2008, 22(5): 200-205.
[24] 黄保健, 甘露, 张之淦. 岩溶地区中子水分仪的野外标定[J]. 中国岩溶, 2000, 19(3): 218-223.
[25] 任伟, 谢世友, 谢德体. 喀斯特山地典型植被恢复过程中的土壤水分生态效应[J]. 水土保持学报, 2009, 23(5): 131-135.
[26] 付同刚, 陈洪松, 张伟, 等. 喀斯特小流域土壤含水率空间异质性及其影响因素[J]. 农业工程学报, 2014, 30(14): 124-131.
[27] 张继光, 陈洪松, 苏以荣, 等. 喀斯特洼地表层土壤水分的空间异质性及其尺度效应[J]. 土壤学报, 2008, 45(3): 544-549.
[28] 容丽, 熊康宁. 花江喀斯特峡谷适生植物的抗旱特征, I: 顶坛花椒根系与土壤环境[J]. 贵州师范大学学报(自然科学版), 2007(4): 5-11, 38.
[29] 邓艳, 蒋忠诚, 李衍青, 等. 广西不同石漠化程度下典型植物水分来源分析[J]. 热带地理, 2015(3): 128-133.
[30] Huang, Y.Q. (2009) Transpiration of Cyclobalanopsis glauca (syn. Quercus glauca) Stand Measured by Sap-Flow Method in a Karst Rocky Terrain during Dry Season. Scientia Horticulturae, 4, 791-801. [Google Scholar] [CrossRef
[31] 邓彭艳, 陈洪松, 聂云鹏, 等. 桂西北喀斯特地区菜豆树和红背山麻杆旱、雨季光合特性比较[J]. 生态学杂志, 2010(8): 24-30.
[32] Peng, X., Dai, Q., Li, C., et al. (2018) Role of Underground Fissure Flow in Near-Surface Rainfall-Runoff Process on a Rock Mantled Slope in the Karst Rocky Desertification Area. Engineering Geology, 243, 10-17. [Google Scholar] [CrossRef
[33] Poesen, J. and Lavee, H. (1994) Rock Fragments in Topsoils: Significance and Processes. Catena, 23, 1-28. [Google Scholar] [CrossRef
[34] Ruiz Sinoga, J.D., Romero Diaz, A. and Ferre Bueno, E. (2010) The Role of Soil Surface Conditions in Regulating Runoff and Erosion Processes on a Metamorphic Hillslope (Southern Spain): Soil Surface Conditions, Runoff and Erosion in Southern Spain. Catena, 80, 131-139. [Google Scholar] [CrossRef
[35] Zhang, J.G., Chen, H.S., Su, Y.R., et al. (2011) Spatial Variability and Patterns of Surface Soil Moisture in a Field Plot of Karst Area in Southwest China. Plant Soil & Environment, 57, 409-417. [Google Scholar] [CrossRef
[36] Li, S., Ren, H.D., Xue, L., et al. (2014) Influence of Bare Rocks on Surrounding Soil Moisture in the Karst Rocky Desertification Regions under Drought Conditions. Catena, 116, 157-162. [Google Scholar] [CrossRef
[37] Fiorillo, F. and Guadagno, F.M. (2012) Long Karst Spring Discharge Time Series and Droughts Occurrence in Southern Italy. Environmental Earth Sciences, 65, 2273-2283. [Google Scholar] [CrossRef
[38] Tan, H., Cai, R., Chen, J., et al. (2017) Decadal Winter Drought in Southwest China since the Late 1990s and Its Atmospheric Teleconnection. International Journal of Climatology, 37, 455-467. [Google Scholar] [CrossRef
[39] Zhang, Z.C., Chen, X., Wang, W., et al. (2007) Analysis of Rainfall Trend and Extreme Events in Guizhou. Earth and Environment, 35, 351-356.
[40] Shi, P., Wu, M., Qu, S., et al. (2015) Spatial Distribution and Temporal Trends in Precipitation Concentration Indices for the Southwest China. Water Resources Management, 29, 3941-3955. [Google Scholar] [CrossRef
[41] Lipiec, J., Kuś, J. and Słowińska-Jurkiewicz, A. (2006) Soil Porosity and Water Infiltration as Influenced by Tillage Methods. Soil & Tillage Research, 89, 210-220. [Google Scholar] [CrossRef