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黄土高原乡级尺度土地利用格局动态变化与生态功能区研究
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摘要
黄土高原在我国区域经济发展中具有重要战略地位,而水土流失严重、生态环境恶劣、加之不合理的土地利用加剧了当地土地资源退化和人民生活贫困。宁南山区是黄土高原的典型代表,如何有效恢复生态环境和摆脱落后面貌,是宁南山区乃至整个黄土高原地区的重要课题。在宁南山区开展土地利用格局变化及其生态环境效应研究,提出土地生态功能区规划,是合理利用土地、改善生态环境和人们生活水平的重要途径。宁南山区土地利用相关研究多集中在小流域尺度,开展乡级尺度的土地利用变化研究对于推广验证小流域的土地利用优化成果,弥补小流域在空间尺度上的局限性,形成“村-乡-县”多尺度全面的土地利用动态变化规律,从根本上解决区域性土地合理利用问题有重要理论与现实意义。
     本文以宁夏自治区固原市河川乡为例,运用“3S”技术,利用早期1:1万地形图与SPOT5遥感影像,在土地资源学与景观生态学理论的指导下,较为全面的研究了乡级尺度的土地利用格局变化及其驱动机制、景观生态效应、土地资源适宜性,提出了生态功能区划方案。论文的主要结果与结论如下:
     (1)土地利用格局变化分析
     对河川乡近三十年包括退耕前1982-2002年和退耕后2002-2008年两个时段的土地利用变化进行研究。1982-2002年,土地利用变化以耕地增加与草地减少最明显,2002-2008年林地增加和耕地减少最显著。整个研究时段内,果园持续增加,体现了果园在河川乡农业发展中的重要地位;建设用地持续增加,但数量小速度慢,说明该地区的社会经济落后与发展缓慢;未利用地持续减少;水域面积变化很小。土地利用类型转化的最主要特征为,1982-2002年以草地向耕地转移为主,2002-2008年以耕地向林/草地转移最为显著。河川乡土地利用程度在退耕前由于盲目开垦草地而增加,在退耕后受到退耕还林草作用而有所下降。利用地学信息图谱方法建立了土地利用类型变化图谱、土地利用增减系列图谱,可以从中直观准确地得到不同土地利用的增减状况和转变方式以及它们的空间分布情况。
     (2)土地利用变化驱动力分析
     土地利用类型随着地形分布有一定的规律性:耕地多分布在中等海拔、坡度0°-15°的区域分布,灌林地在高海拔、15°-35°分布较多,果园和建设用地都选择在0°-8°地势地平区域分布,草地选择坡度大于25°地段分布。土地利用变化的社会经济驱动力呈现阶段性特征,1982-2002年,耕地增加与草地退化主要驱动力是经济,林地增加主要驱动力是科技与政策,果园增加驱动力是科技、政策与经济;2002-2008年,耕地锐减与灌林地大幅度增加的最主要驱动力是政策,果园增加主要驱动力是经济。
     (3)土地利用景观格局变化与生态效应评价
     1982-2008年,河川乡景观格局经历了耕地和草地占共同主导-耕地绝对主导-林地、草地、耕地协调共存的过程,总体上景观优势度下降、多样化提高;景观结构总体上是向可持续方向发展,生态服务价值由1928.43万元增加为3295.61万元。河川乡景观格局与生态服务功能存在地域性,如靠川地分布的骆驼河村、上黄村、明川村和寨洼村景观破碎度、多样性水平、生态服务价值较高。
     (4)不同土地利用方式下的土壤碳氮特征
     土地利用方式是土壤碳氮含量分布及碳密度分布的重要因素。不同的土地利用方式下土壤碳氮含量及有机碳密度均表现为:灌木林地与天然草地碳氮水平较高,耕地较低,人工草地与耕地水平相似。不同土地利用方式的平均有机碳密度分别为:灌木林地6.74 kg m~(-2),天然草地6.32 kg m~(-2),人工草地4.05 kg m~(-2),弃耕地5.69 kg m~(-2),耕地4.11 kg m~(-2),果园4.65 kg m~(-2)。整个河川乡平均有机碳密度为5.67 kg m~(-2),略高于黄土高原平均水平,总碳储量为1148541.66吨。土地利用格局的合理变化对有机碳储量增加有重要意义,灌木林地和天然草地是增加碳汇与控制土壤侵蚀的最有效的土地利用方式,退耕还林对土壤碳储量的增加发挥重要作用。
     (5)土地资源适宜性评价
     选取海拔、坡度、坡向、土壤有机质、土壤侵蚀和水源条件六个指标作为土地适宜性评价因子。按照农、林、牧顺序优先选择,将研究区土地资源划分为五类,高度宜农地占总面积的4.86%,中度宜农地占16.73%,宜林地占3.98%,宜林牧地分布最广,占53.77%,宜牧地比例为20.67%。
     (6)生态功能区划
     在宁夏“六盘山生态经济圈规划”框架下,结合土地利用格局分析、生态系统服务功能评价和土地资源利用适宜性评价结果,将河川乡划分出北山水土保持生态保护区、川地高效生态农业区和南山旱作农业区三个功能区:北山水土保持生态保护区面积13820.53ha,占河川乡总面积的64.13%,地形破碎、土壤侵蚀严重,土地利用方向是恢复植被、保持水土、涵养水源;川地高效生态农业区面积为4627.91ha,占总面积的21.46%,土地较为平整,水肥条件较好,土地利用方向为高效生态农业;南山旱作农业区面积3110.45ha,占总面积的14.4%,土地发展方向为建设旱作基本农田,保障粮食生产。
Loess Plateau has an important strategic position in China's regional economic development, and it has serious soil erosion, bad ecological environment, and poor land use management which exacerbated the degradation of land resources and the poverty of people living. Southern Ningxia is a typical representative of the Loess Plateau. How to restore the ecological environment and get rid of poverty is an important subject for Southern Ningxia and the whole Loess Plateau. Carrying out the study on land use change and its effect on the ecological environment in Southern Ningxia and proposing the ecological function zoning is crucial for rational use of land and improving the eco-environment and people's living standards. Studies on land use in Southern Ningxia focused on the small watershed scale. It is of a great thoretical and practical significance to develop the township scale land use change in order to promote and verify the results of optimizating small watershed land use, make up for the limitations of small watershed scale in space, form a law of "Village - Township - County" multi-scale comprehensive land use dynamic changes, and solve the problem of rational use of regional land fundamentally.
     In this dissertation, taking Hechuan Town in Guyuan City, Ningxia Hui Autonomous Region as an example, using 1:10000 topographic maps and remote sensing image, under the guidance of the technology of GIS and the theory of land resource science and landscape ecology science, and topographic maps, the change of land use pattern, its driving mechanism and ecological effects, suitability and optimized model of land resources, and ecological function zoning at town scale are studied roundly. The main results and conclusions of this paper are as follows:
     (1) Change of land use pattern
     Analysis on change of land use pattern was conducted between the time period of 1982 to 2002 and the time period of 2002 to 2008 in Hechuan Town. Results indicated that the most significant change from 1982 to 2002was the increase of arable land and the decrease of grassland, and that the most significant change from 2002 to 2008 was the increase of forest land and the decrease of arable land. Throughout the study period, the orchard was increasing which reflects its important role in agricultural development in Hechuan Town. The residential area was increasing slowly, indicating that the region's social and economic was poor and its development was slow. In addition, unused land was declining and water area change little. The main types of land use conversion from 1982 to 2002 and from 2002 to 2008 were transferring grassland to arable land and transferring arable land to forest land or grassland, respectively. The degree of land use increased because of the blindfold and excessive grassland reclamation before the Grain for Green project and declined because of the Grain for Green project. With the Geo-informatic Tupu method, the Tupu on land use change and arasing and falling series of land use change was established, from which the characteristics of the increase or decrease of some land use type, the conversion type, and their spatial distribution can be obtained exactly and intuitionisticly.
     (2) Driving forces of land use change
     The distribution of land use pattern has a certain regularity with topographic change: arable land are located in medium altitude and 0°-15°slope, the shrub land are located at high altitudes, 15°-35°slope, the orchards and residential are located at 0°-8°slope and low altitude, and the grassland are located at slope greater than 25°.The characteristics of the socioeconomic driving forces on land use change: in 1982-2002, the main driving force of the increase of arable land and the grassland degradation was economic, the main driving forces of the increase on forest land were science, policy and technology, the main driving force of increasing orchards were technology, policy and economy. In 2002-2008, the main driving force of the decline of arable land and the increase of shrub land was policy; the main driving force of increasing orchards was economy.
     (3) Landscape change and its ecological effects
     The landscape pattern of Hechuan Town from 1982 to 2008 experienced an“arable land and grassland dominated - arable land dominated - coordination of forest, grassland, arable land in propotion”process. The landscape dominance declined, and the diversity increased. The landscape structure developed in the direction of sustainability on the whole. The value of ecosystem services increased from 19,284,300 yuan to 32,956,100 yuan. The landscape patterns and the ecosystem services value existed regional differences. For example, the counties distributed by the flat land, such as Luotuohe, Shanghuang, Mingchuan and Zaiwa, had higher landscape fragmentation, diversity and ecological services value.
     (4) Effect of land use on soil carbon and nitrogen
     Land use is an important factor on the distribution of soil carbon and nitrogen content and carbon density. The characteristic of soil carbon and nitrogen content and organic carbon density under different land uses are as follows: the carbon and nitrogen under shrub land and natural grassland was significantly greater, the carbon and nitrogen under arable land was significantly lower, and the carbon and nitrogen under grassland and arable land were in same level. The organic carbon density under shrubland, natural grassland, artificial grassland, cropland, abandoned cropland, and orchards were 6.74, 6.32, 4.05, 5.69, 4.11, 4.65 kg m~(-2), respectiveily. The organic carbon density in Hechuan Town was 5.67 kg m~(-2), slightly higher than the average level of the Loess Plateau, and the total carbon storage was 1,148,541.66 tons. Rational land use pattern change is of a great significance on the increasing soil organic carbon storage. Shrub land and grassland are the most effective land uses to increase carbon sequestration and control soil erosion. The Grain for Green project plays an important role on the increase of soil carbon stocks.
     (5) Suitability evaluation of land resources
     The six indicators, including altitude, slope, aspect, soil organic matter, soil erosion and water conditions, were selected as the land suitability evaluation factors. In accordance with the order of agriculture, forestry and stockbreeding, the study area was divided into five categories of land resources, including the land highly suitable for agriculture, the land moderately suitable for agriculture, the land suitable for forestry, the land suitable for both forestry and stockbreeding, and the land suitable for stockbreeding, accounting for 4.86%, 16.73%, 3.98%, 53.77% and 20.67%, respectively.
     (6) Ecological function zoning of land use
     Under the Ecological Economic Zone Liupanshan Planning Framework, according to the land use pattern analysis and the results evaluation of ecosystem services and land use suitability evaluation, Hechuan Town was divided into three functional regions: soil and water conservation eco-environmental protection region in north mountain district, high efficiency ecological agriculture region in flat district, and dry farming region in south mountain district. Soil and water conservation eco-environmental protection region in north mountain district areas 13820.53ha, accounting for 64.13% of total area with broken terrain and severe soil erosion, the direction of land use in this region is to restore the vegetation, conserves the soil and water. High efficiency ecological agriculture region in flat district areas 4627.91ha, accounting for 21.46%. The land is flat with good water and fertilizer conditions. The land use direction is to develop the efficient ecological agriculture. Dry farming region in south mountain district areas 3110.45ha, accounting for 14.4 %. The land use direction is to construct basic dry farming land and ensure the food production.
引文
[1]黄秉维,郑度,赵名茶,等.现代自然地理[M].北京:科学出版社, 1999, 195-209.
    [2] IGBP/IHDP. Land-Use and Land-Cover Change Science/Research Plan[R]. IGBP Rep. No. 35 and IHDP Rep. No. 7. 1995.
    [3]陈佑启,杨鹏.国际上土地利用/土地覆盖变化研究的新进展[J].经济地理, 2001, 21(1): 95-100.
    [4]史培军,宫鹏,李晓兵,等.土地利用/覆盖变化研究的方法和实践[M].北京:科学出版社, 2000. 1-60.
    [5]李秀彬.全球环境变化的核心领域-土地利用/覆被变化的国际研究动向[J].地理学报, 1996, 51(6): 553-557.
    [6]汪权方,李家永,陈百明.基于地表覆盖物光谱特征的土地覆被分类系统-以鄱阳湖流域为例[J].地理学报, 2006, 61(4): 359-368.
    [7]摆万奇,柏书琴.土地利用和覆盖变化在全球变化研究中的地位与作用[J].地域研究与开发, 1999, 18(4): 13-16.
    [8]符涂滨,严中伟.全球变化与我国未来的生存环境[M].北京:气象出版社, 1996.
    [9] US-SGCR/CRRN. Our changing plant, the FY 1995 U.S. global change research program[R]. Washington, DC: US-GCRIO, 1996.
    [10]何英彬,陈佑启.土地利用/覆盖变化研究综述[J].中国农业资源与区划, 2004, 25(2): 58-62.
    [11] Briassoulis H. Analysis of land use change: theoretical and modeling approaches [M]. West Virginia University, Morgantown, WV, 2000.
    [12]李学梅,李忠峰.土地利用/覆盖变化研究进展及其意义[J].安徽农业科学, 2008, 36(6): 2462-2464.
    [13]刘英,赵荣钦.土地利用/覆盖变化研究的现状与趋势[J].河北师范大学学报(自然科学版), 2004, 28(3): 310-315.
    [14] UNEP-EAPAP. Land cover assessment and monitoring, volume 1-A, Overall Methodological Framework and Summary[R]. Bankok: UNEP-EAPAP, 1995.
    [15] Otsubo K. Towards land use for global environmental conservation (LU/GEC) project[R]. In: Proceedings of the Work-shop on Land Use for Global Environmental Conservation. Tsukuba, Japan, 1994.
    [16]张新长.基于GIS技术的城市土地利用时空结构演变分析模型研究[D].武汉:武汉大学,2003.
    [17]何春阳,陈晋,陈云浩,等.土地利用/土地覆盖变化混合动态监测方法研究[J].自然资源学报, 2001, 16(3): 255-262.
    [18]路云阁,蔡运龙,许月卿.走向土地变化科学—土地利用/覆被变化研究的新进展[J].中国土地科学, 2006, 20(1): 55-61.
    [19] Ojima D, Lavorel S, Graumich L, et al. Terrestrial human-environment systems: the future of land research in IGBPII [J]. In: Global Change Newsletter Issue No. 50, 2002.
    [20] Moran EF. News on the land project[J]. In: Global Change Newsletter Issue No. 54, 2003.
    [21] Global Land Project(GLP). Science Plan and Implementation Strategy [R]. IGBP Report No. 53 and IHDP Report No. 19. Stockholm: IGBP, 2005.
    [22]石龙宇,卢新,崔胜辉.土地变化的生态效应研究进展[J].中国土地科学, 2008, 22(4): 73-79.
    [23]于兴修,杨桂山.中国土地利用/覆被变化研究的现状与问题[J].地理科学进展, 2002, 21(1): 51-57.
    [24]唐华俊,陈佑启,邱建军,等.中国土地利用/土地覆盖变化研究[M].北京:中国农业科学技术出版社, 2004.
    [25]吴传钧,郭焕成.中国土地利用[M].北京:科学出版社, 1994.
    [26]李毅娜,段汉明.土地利用/覆盖变化研究进展[J].陕西师范大学学报(自然科学版), 2008, 36: 68-70.
    [27]张新长.基于GIS技术的城市土地利用时空结构演变分析模型研究[D].武汉:武汉大学, 2003.
    [28]胡苗.兰州市土地利用变化及驱动力研究[D].兰州:西北师范大学, 2007.
    [29]刘新卫,陈百明,史学正.国内LUCC研究进展综述[J].土壤, 2004, 36(2): 132-135.
    [30]张显峰,崔伟宏.运用RS、GPS和GIS技术进行大比例尺土地利用动态监测的实验研究[J].地理科学进展, 1999, 18(2): 137-145.
    [31]术洪磊,毛赞猷. GIS辅助下的基于知识的遥感影像分类方法研究[J].测绘学报, 1997, 26(4): 329-336.
    [32]骆剑承,周成虎,杨艳.遥感地学智能图解模型支持下的土地覆盖/土地利用分类[J].自然资源学报, 2001, 16(2): 179-183.
    [33]程昌秀,严泰来,朱德海,等. GIS与RS集成的高分辨率遥感影像分类技术在地类识别中的应用[J].中国农业大学学报, 2001, 6(3): 50-54.
    [34]叶庆华,刘高焕,陆洲,等.基于GIS的时空复合体一土地利用变化图谱模型研究方法[J].地理科学进展, 2002, 21(4): 349-357.
    [35] Zhang T.Y, Ye Q.H, Zhou C.H, et a1. Tupu analysis on land use change in the Yellow River Delta and its possible structure by Marcov prediction, Landscape Change and Human Activity, Lanzhou[R]. The 2nd IALE Asia-Pasific Region Conference, China. Sept, 22-25th, 2001.
    [36]摆万奇.深圳市土地利用动态趋势分析[J].自然资源学报, 2000, 15(2): 112-116.
    [37]赵羿,胡远满.土地与景观-理论基础·评价·规划[M].北京:科学出版社, 2005.
    [38]刘湘南,许红梅,曹文.吉林省前郭县土地利用变化空间差异的机制分析[J].地理科学进展, 2001, 20(1): 60-66.
    [39]张明.区域土地利用结构及其驱动因子的统计分析[J].自然资源学报, 1999, 14(4): 381-384.
    [40]叶宝莹,黄方,刘湘南,等.土地利用/覆被变化的驱动力模型研究-以嫩江中上游地区为例[J].东北师大学报自然科学版, 2002, 34(1): 100-104.
    [41]邓祥征,战金艳.中国北方农牧交错带土地利用变化驱动力的尺度效应分析[J].地理与地理科学信息, 2004, 20(3), 64-68.
    [42]邹亚荣,张增祥,周全斌.中国农牧交错区土地利用变化空间格局与土地利用格局变化驱动力分析[J].自然资源学报, 2003, 18(2): 222-227.
    [43]袁俊.湖北省土地利用变化及其驱动力分析[J].国土与自然资源研究, 2003, (4): 33-35.
    [44]王静爱,何春阳.北京城乡过渡区土地利用变化驱动力分析[J].地球科学进展, 2002, 17(2): 201-208.
    [45]杨桂山.长江三角洲近50年耕地数量变化的过程与驱动机制研究[J].自然资源学报, 2001, 16(2): 121-127.
    [46]陈百明.试论中国土地利用和土地覆被变化及其人类驱动力研究[J].自然资源, 1997, (2): 31-36.
    [47]王秀兰.土地利用/土地覆盖变化中的人口因素分析[J].资源科学, 2000, 22(3): 39-42.
    [48]刘纪远,张增祥. 20世纪90年代中国土地利用变化时空特征及其成因分析[J].地理研究, 2003, 22(1): 1-12.
    [49]为欣.城市土地利用变化及其驱动力分析[J].资源环境与工程, 2006, 4(20): 482-486.
    [50]史培军,陈晋,潘耀忠.深圳市土地利用变化机制分析[J].地理学报, 2000, 55(2): 151-160.
    [51]邵晓梅,杨勤业,张洪业.山东省耕地变化趋势及驱动力研究[J].地理研究, 2001, 20(3):298-306.
    [52]摆万奇,阎建忠,张镱锂.大渡河上游地区土地利用/土地覆被变化与驱动力分析[J].地理科学进展, 2004, 23(1): 71-78
    [53]张仁锋,张承中,高文丽.土地利用/覆盖变化研究进展综述[J].甘肃科技, 2007, 23, (6): 122-126.
    [54] Bakkera M.M, Goversb G, Kosmasc C, et al. Soil erosion as a driver of land-use change[J]. Agriculture, Ecosystems and Environment, 2005, 105: 467-481.
    [55]陈佑启, PETER H Verburg,徐彬.中国土地利用变化及其影响的空间建模分析[J].地理科学进展, 2000, 19(2): 116-127.
    [56]赵米金,徐涛.土地利用/土地覆被变化环境效应研究[J].水土保持研究, 2005, 12(1): 43 -46.
    [57]李克让,陈育峰,黄玫,等.气候变化对土地覆被变化的影响及其反馈模型[J].地理学报, 2000, 55(增刊): 57-63.
    [58]康幕谊,江源,石瑞香. NECT样带1984-1996土地利用变化分析[J].地理科学, 2000, 20(2): 115-120.
    [59]王绍强,陈育峰.陆地表层碳循环模型研究及其趋势[J].地理科学进展, 1998, 17(4): 64-70.
    [60]周广胜,王玉辉.土地利用/覆盖变化对气候的反馈作用[J].自然资源学报, 1999, 14(4): 318-322.
    [61]岳文泽,徐丽华.城市土地利用类型及格局的热环境效应研究-以上海市中心城区为例[J].地理科学, 2007, 27(2): 243-248.
    [62]何剑锋,庄大方.长江三角洲地区城镇时空动态格局及其环境效应[J].地理研究, 2006, 25(3): 388-397.
    [63]李昌峰,高俊峰,曹慧.土地利用变化对水资源影响的现状和趋势[J].土壤, 2002, 34(4): 191-197.
    [64]阎伍玫,陈非星.巢湖流域不同土地利用类型地表径流污染特征研究[J].长江流域资源与环境, 1998, 7(3): 274-277.
    [65]杨金玲,张甘霖,张华,等.丘陵地区流域土地利用对氮素径流输出的影响[J].环境科学, 2003, 24(1): 18-23.
    [66]梁涛,张秀梅,章申,等.西笤溪流域不同土地类型下磷素随暴雨径流的迁移特征[J].环境科学, 2003, 24(2): 35-40.
    [67]李俊然,陈利顶,傅伯杰,等.于桥水库流域地表水非点源N时空变化特征[J].地理科学, 2002, 22(2): 238-242.
    [68]史培军,袁艺,陈晋.深圳市土地利用变化对流域径流的影响[J].生态学报, 2001, 21(7): 1041-1049.
    [69]曹慧,杨浩,孙波,等.太湖流域丘陵地壤养分的空间变异[J].土壤, 2002, 34(4): 201-205.
    [70]傅伯杰,马克明,赝华峰.黄土丘陵区土地利用结构对土壤养分分布的影响[J].科学通报, 1998, 43(22): 2444-2447.
    [71]傅伯杰,陈利顶,马克明.黄土丘陵区小流域土地利用变化对生态环境的影响-以延安市羊圈沟流域为例[J].地理学报, 1999, 54(3): 241-246.
    [72]郭旭东,傅伯杰,陈利顶,等.低山丘陵区土地利用方式对土壤质量的影响-以河北省遵化市为例[J].地理学报, 2001, 56(4): 447-455.
    [73]蔡崇法,丁树文,张光远,等.三峡库区紫色土坡地养分状况及养分流失[J].地理研究, 1996, 15(3): 77-84.
    [74]张桃林,鲁如坤,李忠佩.红壤丘陵区土壤养分退化与养分库重建[J].长江流域资源与环境, 1998, 7(1): 18-24.
    [75]丘君,陈利顶,傅伯杰. LUCC对生物多样性影响中国地理学会自然地理专业委员会编.土地覆被变其环境效应[M].北京:星球地图出版社, 2002.
    [76]尹发能,王学雷,余璟.大九湖土地利用变化及其对湿地生态环境的影响研究[J].华中师范大学学报(自然科学版), 2007, 41(1): 148-151.
    [77]吕士成,陈浩,杜进进.盐城自然保护区人工湿地对水鸟分布的影响[J].农村生态环境, 1996, 12(3): 15-17.
    [78]黄青,孙洪波,王让会,等.干旱区典型山地—绿洲—荒漠系统中绿洲土地利用/覆盖变化对生态系统服务价值的影响[J].中国沙漠, 2007, 27(1): 76-81.
    [79]张宝雷,张淑敏,周启刚.土地利用和生态系统服务功能变化研究-以三峡库区大宁河流域为例[J].长江流域资源与环境, 2007, 16(2): 181-185.
    [80]李晓文,方精云,朴世龙.近10年来长江下游土地利用变化及其生态环境效应[J].地理学报, 2003, 58(5): 659-667.
    [81]温仲明,焦峰,张晓萍等.纸坊沟流域近60年来土地利用景观变化的环境效应[J].生态学报, 2004, 24(9): 1903-1909.
    [82]彭建,王仰麟,张源等.滇西北生态脆弱区土地利用变化及其生态效应-以云南省永胜县为例[J].地理学报, 2004, 59(4): 629-638.
    [83]王根绪,刘进其,陈玲.黑河流域典型区土地利用格局变化及影响比较[J].地理学报, 2006, 61(4): 339-348.
    [84]刘全友,童依平.北方农牧交错带土地利用现状对生态环境变化的影响-以内蒙古多伦县为例[J].生态学报, 2003, 23(5): 1025-1030.
    [85]李晓文,方创琳,黄金川,等.西北干旱区城市土地利用变化及其区域生态环境效应-以甘肃河西地区为例[J].第四纪研究, 2003, 23(3): 280-290.
    [86]史培军,潘耀忠,陈晋,等.深圳市土地利用/覆盖变化与生态环境安全分析[J].自然资源学报, 1999, 14(4): 293-299.
    [87]王秀兰,包玉海.土地利用动态变化研究方法探讨[J].地理科学进展, 1999, 18(1): 81-87.
    [88]唐华俊,吴文斌,杨鹏,等.土地利用/土地覆被变化(LUCC)模型研究进展[J].地理学报, 2009, 64(4): 456-468.
    [89] Verburg P.H, Soepboer W, Limpiada R, et al. Modeling the spatial dynamics of regional land use: The CLUE-S model[J]. Environmental Management, 2002, 30: 391-405.
    [90] Pontius J.R.G, Cornell J.D, Hall C.A.S. Modeling the spatial pattern of land-use change with GEOMOD2: Application and validation for Costa Rica[J]. Agriculture, Ecosystems and Environment, 2001, 85: 191-203.
    [91] Goldstein N.C, Candau J.T, Clarker K.C. Approaches to simulating the"March of bricks and mortar"[J]. Computers, Environment and Urban Systems, 2004, 28: 125-147.
    [92]全斌.黄土高原六盘山区土地利用变化及生态农业模式比较研究[D].中国科学院研究生院, 2007.
    [93] Harmon R.S. and Dow W.W. Landscape Erosion and Evolution Modeling[M]. Kluwer Academic/Plenum Publishers, New York. 2001, 1-13.
    [94]肖笃宁,李秀珍.景观生态学的学科前沿与发展战略[J].生态学报, 2003, 23(8): 1615-1621.
    [95]邬建国.景观生态学中的十大研究论题[J].生态学报, 2004, 24(9): 2074-2076.
    [96]孙彦伟,卢荣安,姜广辉.区域土地持续利用规划的景观生态学思维[J].生态经济, 2005, 3: 56-59.
    [97] Bailey R.C., Reynoldson T.B., Yates A.G., et al. Integrating stream bioassessment and landscape ecology as a tool for land use planning[J]. Freshwater Biology, 2007, 52: 908-917.
    [98] Dongjie G., Weijun G., Kazuyuki W., et al. Land use change of Kitakyushu based on landscapeecology and Markov model [J]. Journal of Geographical Sciences, 2008, 18: 455-468.
    [99]邬建国.景观生态学-格局、过程、尺度与等级[M].北京高等教育出版社, 2000.
    [100]傅伯杰,陈利顶,王军,等.土地利用结构与生态过程[J].第四纪研究, 2003, 23(3): 247-255.
    [101] Centeri C., Herczeg E., Vona M., et al. The effects of land-use change on plant-soil-erosion relations, Nyereg Hill, Hungary [J]. Journal of Plant Nutrition and Soil Science-Zeitschrift Fur Pflanzenernahrung Und Bodenkunde, 2009, 172(4): 586-592.
    [102] Buse A. Environmental-effects of land use change, as identified by habitat recording- A case study in the Llyn Peninsula, Wales [J]. Journal of Environmental Management, 1992, 35(2): 131-135.
    [103] Turner B.L.II, Clark W.C., Kates R.W., et al。The earth as transformed by human action: global and regional changes in the biosphere over the past 300 years[M]. Cambridge: Cambridge University Press, 1990.
    [104]吴钦孝,杨文治.黄土高原植被建设与持续发展[M].北京:科学出版社, 1998: 1-15.
    [105]傅伯杰,陈利顶,邱扬,等.黄土丘陵沟壑区土地利用结构与生态过程[M].北京:商务印书馆出版社, 2002.
    [106] Zheng F.L. Effect of vegetation changes on soil erosion on the Loess Plateau[J]. Pedosphere, 2006, 16, 420-427.
    [107]李锐,杨文治,李壁成,等.中国黄土高原研究与展望[M].北京:科学出版社, 2008: 612-632.
    [108]王宗明,张柏,宋开山,等.基于地形图与知识规则的土地利用信息提取[J].地球信息科学, 2008, 10(1): 67-73.
    [109] Prol-ledesma R.M., Uribe-alcantara E.M., Diaz-molina O. Use of cartographic data and landsat TM images to determine land use change in the vicinity of Mexico city[J]. Remote Sensing of Environment, 2002, 23 (9): 1927-1933.
    [110] Yuan D Elvdge. Land cover change detection pilot study: Washington DC area experiments[J]. Remote Sensing of Environent, 1999, (15): 66-178.
    [111] Xiao J., Shen Y., Ge J.,ea tl. Evaluating urban expansion and land use change in Shijiazhuang, China, by using GIS and remote sensing. Landscape and Urban Planning, 2006, 75: 69-80.
    [112]张建斌,唐菊兴,刘登忠.卫星遥感图像空间分辨率适用性分析[J].地球科学与环境学报, 2006, 28(1): 79-83.
    [113]初艳锋,李二森,卢俊,等.卫星影像空间分辨率与成图比例尺的适应性分析[J].海洋测绘, 2007, 27(4): 47-50.
    [114]潘家文,朱德海,严泰来,等.遥感影像空间分辨率与成图比例尺的关系应用研究[J].农业工程学报, 2005, 21(9): 124-128.
    [115]李乔,刘春.数字土地利用现状图的制图概括[J].测绘工程, 2002, 9(2): 59-63.
    [116]刘盛和,何书金.土地利用动态变化的空间分析测算模型[J].自然资源学报, 2002, 17(5): 533-540.
    [117]刘纪远,布和敖斯尔.中国土地利用变化现代过程时空特征的研究-基于卫星遥感数据[J].第四纪研究, 2002, 20(3): 229-239.
    [118]赖彦斌,徐霞,王静爱. NSTEC不同自然带土地利用/覆盖格局分析[J].地球科学进展, 2002, 17(2): 215-220.
    [119]王思远,张增祥,周全斌,等.基于遥感与GIS技术的土地利用时空特征研究[J].遥感学报, 2002, 6(3): 223-228.
    [120]喻红,曾辉,江子瀛.快速城市化地区类型组分在地形梯度上的分布特征研究[J].地理科学, 2001, 21(1): 64-69.
    [121]斯钧浪,齐伟,曲衍波,等.胶东山区县域土地利用在地形梯度上的分布特征[J].应用生态学报, 2009, 20(3): 679-685.
    [122]罗云云,李瑞雪,屈明.重庆石碗溪小流域坡度和高程对土地利用及经济发展的影响[J].山地学报, 2004, 22(2): 254-258.
    [123]孙彦伟,卢荣安,姜广辉.区域土地持续利用规划的景观生态学思维[J].生态经济, 2005, 3: 56-59.
    [124]李哈滨,伍业纲,刘建国.景观生态学的数量研究方法[M].中国科学技术出版社,北京, 1992.
    [125] Comber A.J., Birnie R.V., Hodgson M. Using landscape metrics to model land cover change [J]. Quantitative Approaches to Landscape Ecology, 2000, 143-161, 194.
    [126] Herzog F., Lausch A. Supplementing land-use statistics with landscape metrics: Some methodological considerations[J]. Environmental Monitoring and Assessment, 2001, 72 (1): 37-50.
    [127]卢玲.黑河流域景观结构与景观变化研究[D].中国科学院寒区旱区环境与工程研究所硕士学位论文, 2000: 1-18.
    [128]赵羿,李月辉.实用景观生态学[M].北京:科学出版社, 2001, 92-97.
    [129] Costanza R., Arge D.R, Groot D.R., et al. The value of the world’s ecosystem services and natural capital[J]. Nature, 1997, 387: 253-260.
    [130]彭建,王仰麟,张源,等.滇西北生态脆弱区土地利用变化及其生态效应-以云南省永胜县为例[J].地理学报, 2004, 59(4): 629-638.
    [131]邓伟,杨华,崔艳君.重庆主城区近30年土地利用变化的生态环境效应评价[J].水土保持研究, 2010, 17(3): 232-235.
    [132]郝慧梅,任志远,薛亮,等.基于3S的榆林市土地利用/覆盖变化生态效应定量研究[J].地理科学进展, 2007, 26(3): 96-106.
    [133]谢高地,鲁春霞,冷允法,等.青藏高原生态资产的价值评估[J].自然资源学报, 2003(2): 189-196.
    [134]谢高地,鲁春霞,成升魁.全球生态系统服务价值评估研究进展[J].资源科学, 2001, 23(6): 5-9.
    [135]肖玉,谢高地,安凯.莽措湖流域生态系统服务功能经济价值变化研究[J].应用生态学报, 2003, 14(5): 676-680.
    [136] Gregorich E.G., Carter M.R., Angers D.A., et al. Toward minimum data set to assess soil organic-matter quality in agricultural soils[J]. Canadian Journal of Soil Science, 1994, 74, 885-901.
    [137] Stevenson F.J., Cole M.A. Cycles of Soil[M]. 2nd ed. Wiley, New York, 1999.
    [138] IPCC. Land-use, land-use change, and forestry. In: Watson, R. T. , Noble, I. R. , Bolin, B. R. , Ravindranath, N. H. , Verardo, D. J. , Dokken, D. J. (Eds. ), Land-use, Land-use Change, and Forestry, A Special Report of the Intergovernmental Panel on Climate Change (IPCC)[R]. Cambridge University Press, UK, 2000, 1-51.
    [139]李文萍,刘兴年,等.浅谈黄土高原地区水土流失灾害及其防治[J].四川水利, 2003, (4): 37-38.
    [140]付会芳.黄土高原水土流失及其防治措施[J].水土保持研究, 1997, 4(1): 161-162.
    [141] Ritsema C.J. Introduction: soil erosion and participatory land use planning on the Loess Plateau in China[J]. Catena, 2003, 54, 1-5.
    [142] Yu D., Shi X., Wang H., Sun W., et al. 2007. National scale analysis of soil organic carbon storage in China based on Chinese soil taxonomy[J]. Pedosphere, 17, 11-18.
    [143]安韶山,黄懿梅,刘梦云,李壁成.宁南宽谷丘陵区土壤肥力质量对生态恢复的响应[J].水土保持研究, 2005, 12(3): 22-26.
    [144]傅伯杰,陈利顶,马克明.黄土丘陵区小流域土地利用变化对生态环境的影响[J].地理学报, 1999, 54(3): 241-246.
    [145]张俊华,常庆瑞,贾科利,等.黄土高原植被恢复对土壤肥力质量的影响研究[J].水土保持学报, 2003, 17(4): 38-42.
    [146]安韶山,黄懿梅,李壁成,等.用典范相关分析研究宁南宽谷丘陵区不同土地利用方式土壤酶活性与肥力因子的关系[J].植物营养与肥料学报, 2005, 11(5): 704-709.
    [147]南京农业大学.土壤农化分析[M].北京:农业出版社, 1985.
    [148] Chien Y.J, et al. Geostatistics analysis of soil properties of mid-west Taiwan soils[J]. Soil Sci. , 1997, 162: 291-298.
    [149] VanMeirvenne M., Pannier J., Hofman G., and Louwagie G. Spatial and temporal changes of soil C after establishment of a pasture on along-term cultivated vertisol (Martinique)[J]. Geoderma, 1996, 94, 43-58.
    [150] Wang Z.M., Zhang B., Song K.S., Liu D.W., et al. Spatial variability of soil organic carbon under maize monoculture in the Song-Nen Plain, Northeast China[J]. Pedosphere, 2010, 20(1), 80-89.
    [151] Wei J.B. , Xiao D.N., Zhang X.Y., et al. Spatial variability of soil organic carbon in relation to environmental factors of a typical small watershed in the black soil region, Northeast China[J]. Environmental Monitoring and Assessment, 2006, 121, 597-613.
    [152] Fu X..L., Shao M.A., Wei X.R., et al. Soil organic carbon and total nitrogen as affected by vegetation types in Northern Loess Plateau of China[J]. Geoderma1, 2010, 55, 31-35.
    [153]齐雁冰,黄标,顾志权,等.长江三角洲典型区农田土壤碳氮比值的演变趋势及其环境意义[J].矿物岩石地球化学通报, 2008, 27: 50-56.
    [154] Cambardella C.A., Moorman T.B., Novak J.M., et al. Field-scale variability of soil properties in Central Iowa soils[J]. SoilSci. Soc. Am. J., 1994, 58, 1501-1511.
    [155]宋治清,王仰麟,丁艳,等.市域生态功能区划与可持续发展研究-以深圳市为例[J].资源科学, 2004, 26(5): 117-124.
    [156]贾良清,欧阳志,赵同谦,等.安徽省生态功能区划研究[J].生态学报, 2005, 25(2): 254-260.
    [157]徐晓芳,王让会,李锦,等.基于3S的极端干旱区县域生态功能区划研究-以新疆鄯善县为例[J].干旱区资源与环境, 2007, 21(11): 85-89.
    [158]燕乃玲,赵秀华,虞孝感.长江源区生态功能区划与生态系统管理[J].长江流域资源与环境, 2006, 15(5): 598-603.
    [159] Daily G.C. Natures: Societal Dependence on Natural Ecosystems [M]. Washington D C: Island press, 1997.
    [160]赵军,刘高焕,傅新.基于生态功能区划的黄河三角洲土地资源优化配置[J].地理科学进展, 2010, 29(4): 489-494.
    [161]胡孟春,马荣华.黑河流域生态功能区划遥感制图方法[J].干旱区资源与环境, 2003, 17(1): 49-54.
    [162]徐昔保,张建明,祁永安,等.基于3S的石羊河流域生态功能区划研究[J].干旱区研究, 2005, 22(1): 41-44.

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