基于AnnAGNPS模型的三峡库区秭归县非点源污染输出评价

非点源(NPS)污染已成为全球关注的环境问题。由于NPS特点、实验手段和监测数据的局限,其研究多采用数学模型进行时间和空间模拟。模型模拟提供了一种成本低效率高的手段来评定区域非点源污染。选择连续农业非点源污染AnnAGNPS(Annualized AGricultural Non-Point Source)模型,构建该模型数据库,模拟秭归县黑沟、兰陵溪、杉木溪等3条典型流域和县域径流、泥沙和营养物质的输出。结果表明：AnnAGNPS模型对3条典型流域的径流模拟能力高于对泥沙和养分的模拟,径流模拟误差均在可接受范围之内,说明模型中采用的径流预测(SCS曲线)法对研究区的地理气候条件是适用的;对3条典型流域泥沙输出模拟误差较高,对氮磷等养分输出模拟的误差最高,通过调整RUSLE和HUSLE等子模型的输入参数来减小泥沙模拟误差;对小型降雨径流事件,模型泥沙、养分模拟误差有偏大趋势,对较大降雨径流事件,模型泥沙和养分模拟误差有偏小趋势;2006年秭归县县域模型模拟的地表径流量为363 mm,泥沙输出为19.6 t/hm2,总氮输出为122 kg/hm2,总磷输出为28 kg/hm2,有机碳输出为581 kg/hm2,模拟结果与相关文献研究和政府统计数据较为相符;AnnAGNPS模型对NPS污染物输出模拟具有一定的不确定性,但作为一个较好的高级农业流域管理工具,该模型可以在三峡库区地理气候条件下使用。     

流域单元景观格局与农业非点源污染的关系

农业非点源污染日益成为影响地表环境的主要污染方式之一,正确理解景观格局和农业非点源污染过程的关系是进一步认识农业非点源污染发生机制的关键。本文应用去趋势典范对应分析方法（DCCA）对石头口门水库控制流域13个流域单元的景观格局与农业非点源污染关系进行定量分析。结果表明:DCCA排序前2轴分别与森林比率、植被指数、景观聚集度指数、多样性指数和耕地及居民建设用地比率显著相关,累计解释了景观格局与农业非点源污染关系的92%,证明此方法对研究目标具有较高显示度。各流域单元农业非点源污染养分径流输出特征沿景观因子梯度具有明显空间变异。     

苕溪流域非点源污染特征及其影响因子

应用土壤水体评价模型（SWAT）对苕溪流域径流量、泥沙、营养盐负荷进行模拟计算,分析了2008年苕溪流域非点源污染的时空分布特性.结果表明：苕溪流域非点源污染单位面积产生量表现为北部高于南部、东部高于西部、中部地区最少;耕地是泥沙和污染物产生的主要来源,其单位面积负荷远大于其他土地利用类型;产流量、产沙量与降水量呈显著正相关关系（P<0.05）,雨季(6-9月)的营养盐输出大于旱季(12月至次年3月);平均坡度与泥沙负荷、有机氮负荷及硝态氮负荷呈显著相关关系（P<0.05）.     

基于增强回归树的流域非点源污染影响因子分析

地表水的非点源污染在点源污染不断得到控制的前提下已经成为水环境污染的首要问题.非点源污染影响因子的复杂性及不确定性一直是流域非点源污染研究的重点和难点.本文利用SWAT(Soil and Water Assessment Tool)模型,以辽河子流域汎河流域为例,模拟了2003—2012年的非点源污染状况,对其空间分布状况进行了分析,并应用增强回归树的方法定量分析各种影响因子(坡度、土地利用类型、高程和土壤类型)对该流域非点源污染的贡献率.结果表明: 在汎河流域,非点源污染呈现较高的空间异质性,其中总氮的空间分布差异较大,总磷的空间分布差异较小.坡度因子与载体泥沙、总氮和总磷均呈极显著正相关关系(P<0.01),对泥沙和总磷有显著影响,其贡献率分别为46.5%、38.2%;土地利用因子对载体泥沙、总磷的负荷量有重要影响,其贡献率分别达到27.2%、35.3%;高程较低、坡度较缓的耕地地区易产生较高的总磷负荷量;褐色土壤最易流失总磷,而草甸土易流失总磷,且易受泥沙侵蚀.本研究利用增强回归树模型克服了流域非点源污染影响因子的复杂性,可加深对非点源污染产生机制的理解.     

鄱阳湖流域泥沙流失及吸附态氮磷输出负荷评估

水土流失是吸附态氮磷输出负荷的主要方式,也是非点源污染评估的重要环节。鄱阳湖流域水土流失及其所带来的泥沙和吸附态氮磷等营养盐将直接影响到鄱阳湖的生态功能,进而影响着长江中下游水环境安全。科学估算鄱阳湖赣江、抚河、信江、饶河、修河等五大流域的土壤侵蚀量和吸附态氮、磷的输出负荷,将为鄱阳湖流域农业非点源污染控制及鄱阳湖生态建设和环境保护提供理论依据。以2007年全国第一次农业污染源普查数据和2007年江西省土壤质量调查数据为基础,利用RUSLE方程和GIS的空间统计功能,对江西省境内鄱阳湖流域的土壤侵蚀量和吸附态氮、吸附态磷的输出负荷进行估算。结果表明：基于RUSLE得到的2007年鄱阳湖五大流域输沙模数比较可信,鄱阳湖流域内泥沙、吸附态氮、吸附态磷的年输出负荷分别为1245183t、3383t和73t,其中赣江流域吸附态氮磷的年输出负荷最大,占鄱阳湖全流域的58.1%,抚河、饶河、信江、修河等分别占11.2%、7.2%、11.3%和12.2%。与流域内农业污染源总氮、总磷排放量相比较,尽管流域尺度内泥沙的输出负荷相对较大,但吸附态氮、磷的输出负荷较小,应该不是鄱阳湖水污染中总氮和总磷等营养盐的主要来源。     

中国东北地区非点源污染研究进展

为掌握东北地区非点源污染研究动态和明确研究中存在的问题和不足,对近20年（1991-2008年）东北地区有关非点源污染研究成果进行检索、分类和统计分析,以便更好地进行区域水环境治理和污染防治.东北地区非点源污染研究总体呈增加趋势;研究内容包括水环境污染源调查分析与评价、污染负荷量化、机理探索、模型模拟和污染防治5类;研究对象包括氮、磷、泥沙、农药和重金属;经验方法估算污染负荷较多,机理模型应用成功实例较少;研究性论文中以农业非点源污染较多,城市非点源污染较少;治理措施停留在水土保持措施层面上,缺乏对水土保持措施的优选评价和对最佳管理措施的评价研究.目前,东北地区非点源污染研究处在理论探索阶段,非点源污染是否是主要污染源还存在争议.今后应着力于措施应用、评价和基础数据收集及区域非点源污染物的确定和污染负荷的量化研究;尝试新技术和多领域交叉合作,为区域水环境治理提供科学依据.     

农业非点源污染控制中的最佳管理措施及其发展趋势

农业非点源污染是最主要的一类非点源污染,容易造成水体的富营养化,降低环境的质量,已经成为构成目前水质环境恶化的一大威胁。农业非点源污染具有随机性、广泛性等特点,因此对农业非点源污染的控制相对比较困难。最佳管理措施通过工程措施、耕种措施和管理措施共同作用控制农业非点源污染,可以取得良好的经济效益、社会效益和环境效益。其中工程措施有梯田与山边沟,草沟与植被过滤带、人工湿地、节水灌溉系统等,耕种措施有保护性耕作、等高线种植、合理轮作等,管理措施包括有害生物综合治理、综合肥力管理、农田灌溉制度等。最后,本文还对最佳管理措施的发展趋势作了展望。     

基于模型的农业非点源污染最佳管理措施效率评估研究进展

随着点源污染的逐步控制,农业非点源污染已成为世界范围内关注的热点,由于其特有的时空异质性特点导致对其进行有效控制较为困难,最佳管理措施(BMPs,Best Management Practices)是实现流域农业非点源污染控制的有效手段,对拟实施的BMPs效率进行评估是实施流域非点源污染BMPs配置的前提。通过模型模拟的方法可对拟采用的不同措施的削减效率及经济成本进行评估以获取最具成本-效益的BMPs空间配置方案,为措施有效选择提供依据。通过对多种模型在工程型和管理型BMPs评估方面的研究进行论述表明,通常概念化模型多用于对污染源控制类措施进行评估,而机制类模型则可用于对不同时空尺度下的过程控制类BMPs进行评估;措施效率发挥的时间滞后性及模型模拟不确定性是模型模拟过程中需要重点考虑的问题,可通过增加野外监测点数量、监测频率、优化监测点位置并选择合适的评估指标以降低模型评估BMPs过程中滞后效应的影响;此外BMPs实施时间与空间位置的不匹配、时空尺度异质性、污染物形态及生态系统服务功能转换风险均需在BMPs评估过程中加以考虑。模型模拟是BMPs效率评估(包括非点源污染关键源区的时空识别)、污染物迁移转化以及成本效益分析的有效工具,同时对于流域非点源污染管理控制及BMPs实施利益相关者有效参与问题的分析也具有重要意义。     

最佳管理措施评估方法研究进展

针对流域非点源污染的关键源区,进行最佳管理措施(BMPs)的配置,是非点源污染控制的有效途径.污染削减效率的准确识别对于BMPs在目标流域内的有效实施具有非常重要的意义.通过综合对比和分析实地监测、养分平衡、风险评估以及模型模拟等四类最佳管理措施评估方法的有效性、特点、适用条件及其局限性,得出以下结论:养分平衡法较为简便且易于使用,相较于其他方法,所需时间短且又可以消除评估效果的滞后效应,但对污染物削减的时间效应和传输过程影响考虑较少.风险评估和模型模拟方法可以更好地应对不同时空尺度下削减措施效率的评估,但需要大量实测数据的支持,同时模型模拟中普遍存在的时空不确定性影响很难消除.由于各种评估方法都有一定的适用条件,单一方法难以有效地完成评估目标,需要综合应用各类方法,才能最大程度地发挥这些方法的潜在功能和有效性,进而实现BMPs措施使用的成本-效益目标.     

流域尺度农业磷流失危险性评价与关键源区识别方法

农业非点源磷污染是我国农村水环境面临的严重问题之一,由于非点源污染治理难度大,所以识别流域内磷流失的关键源区成为非点源磷污染评价的主要目的.本文在分析流域尺度磷流失危险与分级方案的基础上,根据Gburek等提出的方法,建立了适合我国北方农业区流域尺度磷流失危险评价、分级与关键源区识别的方法.修正的流域尺度磷分级方案重点选取了8个评价因子,分别赋予不同的权重;每个因子的危险性等级根据我国的行业标准和实际情况进行了调整.评价得到的"高"危险性区域就是流域内磷流失的关键源区.这一分级评价方案考虑了数据的可获得性和评价的定量性,在确定各因子时注重与GIS技术、地统计学等方法的结合,具有较强的可操作性和实用性.     

Effect of vegetation on runoff-sediment yield relationship at different spatial scales in hilly areas of the Loess Plateau, North China

Whether vegetation reduces soil loss by reducing runoff volume or rather by changing runoff-sediment yield relationship has received little attention. Base on the observed data from monitoring stations and the published data from other research, this issue is addressed at different scales in hilly areas of the Loess Plateau, North China. At the plot scale, vegetation helps reduce soil loss not only by reducing runoff volume, but also by changing the runoff-sediment yield relationship, resulting that the sediment-reduction rate is higher than the runoff-reduction rate. At the watershed scale, gully erosion and mass wasting process are dominant. Vegetation measures are insufficient to control local mass movement, implying that sediment availability remains high even after vegetation is established. It is also hard for slope vegetation to change the capacity of the sediment transport system at the watershed scale. Therefore, vegetation cannot change the runoff-sediment yield relationship at the watershed scale. This implies that vegetation reduces sediment yield only by reducing runoff volume and the sediment-reduction rate approximates the runoff-reduction rate at the watershed scale. Other slope measures for soil conservation such as terraces are considered to have the same effect on the runoff-sediment yield relationship as the vegetation. Several case studies involving different spatial scales are presented and confirm this conclusion.     

Effect of vegetation on runoff-sediment yield relationship at different spatial scales in hilly areas of the Loess Plateau, North China

Whether vegetation reduces soil loss by reducing runoff volume or rather by changing runoff-sediment yield relationship has received little attention. Base on the observed data from monitoring stations and the published data from other research, this issue is addressed at different scales in hilly areas of the Loess Plateau, North China. At the plot scale, vegetation helps reduce soil loss not only by reducing runoff volume, but also by changing the runoff-sediment yield relationship, resulting that the sediment-reduction rate is higher than the runoff-reduction rate. At the watershed scale, gully erosion and mass wasting process are dominant. Vegetation measures are insufficient to control local mass movement, implying that sediment availability remains high even after vegetation is established. It is also hard for slope vegetation to change the capacity of the sediment transport system at the watershed scale. Therefore, vegetation cannot change the runoff-sediment yield relationship at the watershed scale. This implies that vegetation reduces sediment yield only by reducing runoff volume and the sediment-reduction rate approximates the runoff-reduction rate at the watershed scale. Other slope measures for soil conservation such as terraces are considered to have the same effect on the runoff-sediment yield relationship as the vegetation. Several case studies involving different spatial scales are presented and confirm this conclusion.     

Nutrient budgets and biogeochemistry in an experimental agricultural watershed in Southeastern China

During a two-year field study, an annual nutrient budget and cycles were developed for a small agricultural watershed. The study emphasized the integrated unit of the watershed in understanding the biogeochemistry. It was found that the total nutrient input was 39.1× 10⁴ kg nitrogen and 3.91×10⁴ kg phosphorus in the year 1995, of which the greatest input of nutrients to the watershed was chemical fertilizer application, reaching 34.7×10⁴ kg (676 kg/ha) nitrogen and 3.88×10⁴ kg (76 kg/ha) phosphorus. The total nutrient output from the watershed was 13.55×10⁴ kg nitrogen and 0.40×10⁴ kg phosphorus, while the largest output of nitrogen was denitrification, accounting for 44.1% of N output; the largest output of phosphorus was sale of crops, accounting for 99.4% of P output. The results show that the nutrient input is larger than output, demonstrating that there is nutrient surplus within the watershed, a surplus which may become a potential source of nonpoint pollution to area waters. The research showed that both denitrification and volatilization of nitrogen are key ways of nitrogen loss from the watershed. This suggests that careful management of fertilizer application will be important for the sustainable development of agriculture.The research demonstrated that a multipond system within the watershed had high retention rate for both water and nutrients, benefiting the water, nutrient and sediment recycling in the terrestrial ecosystem and helping to reduce agricultural nonpoint pollution at its source. Therefore, this unique watershed system should be recommended due to its great potential relevance for sustainable agricultural development.     

模拟降雨下喀斯特坡耕地土壤养分输出机制

喀斯特区坡耕地水土及养分流失不仅是该区土地质量退化、土地生产力衰退主要原因,同时也是该区地下水质污染的重要因素。为揭示喀斯特坡耕地地表和地下二元空间结构下的土壤养分流失机制,以喀斯特坡耕地为研究对象,通过模拟其地表微地貌及地下孔(裂)隙构造特征,采用人工模拟降雨试验研究不同雨强下喀斯特坡耕地地表及地下水土及其氮、磷、钾流失特征。结果表明:(1)小雨强(50mm/h)和中雨强下(70mm/h),喀斯特坡耕地坡面产流主要以地下产流为主;大雨强下(90mm/h),地表径流高于地下径流;产沙方式则表现为由小雨的地表和地下产沙并重到中大雨强的地表产沙为主的一个转变过程。(2)在降雨侵蚀过程中,径流各养分输出浓度均表现出一定的初期冲刷效应,受土壤吸附作用影响,雨强对全钾(TK)和全氮(TN)的影响较全磷(TP)明显。(3)地表径流、地表泥沙和总泥沙各养分输出负荷均随雨强增大而增加,坡面径流泥沙总的TK输出负荷以泥沙为主,而TN和TP输出负荷则以径流为主;TP和TN在径流的输出负荷上以地下径流输出为主(其中TP地表负荷比在11.6%—46.2%,TN在7.0%—48.5%之间),而TK则以二者并重(地表负荷比在43.5%—57.0%之间);各养分在泥沙的输出负荷上则均以地表泥沙流失为主,其负荷比均在54.5%以上。研究结果可为喀斯特区坡耕地水土流失及养分流失的源头控制提供基本参数和科学依据。     

Optimal conservation planning of multiple hydrological ecosystem services under land use and climate changes in Teshio river watershed,northernmost of Japan

Most anthropogenic activities impacted on water quality and quantity, and further impacted on ecosystem services (ESs) in watershed are related to land use and climate changes those may cause losses of ecosystem functions. Effective information regarding ESs and their optimal priority conservation planning responded to land use and climate changes provide useful support for diverse stakeholders in ESs planning, management and policies. This study integrated the approach of spatially explicit ESs (water yield, inorganic nutrient, organic nutrient and sediment retentions) by using hydrology and material flow model (Soil and Water Assessment Tools, SWAT model) into systematic conservation of hydrological ESs according to land use and climate changes in Teshio watershed located in the north of Hokkaido, Japan. We investigated the spatial patterns and the hotspots of ESs changes to determine the spatial pattern of changes in systematic conservation optimal area of ES protection in terms of ESs protection targets. Under the land use and climate change scenarios, the forest land use significantly affected on the water yield, sediment, organic-Nitrogen (N) and organic-Phosphorous (P) retentions. The agricultural land (paddy and farmland fields) impacted on the inorganic-N and inorganic-P retentions. We applied the systematic conservation model (MARXAN model) to optimize the area for management of hydrological ESs satisfied the protection targets (30% and 50% of potential maximum ESs values among all scenarios) in all and individual ecosystem services, respectively. The simulated results indicated that the areas of spatial optimal ESs protection for all hydrological ESs were totally different from those for individual ESs. For bundles of ESs, the optimal priority conservation areas concentrated in southwest, north, and southeast of this watershed, which are related to land use, topography and climate driving factors. These places could guarantee ESs sustainability from both environmental protection and agricultural development standpoints. The priority conservation area turned more compact under climate change because the increased precipitation and temperature increased ESs amount. For individual ESs, the optimal priority conservation areas of water yield, sediment retention and organic nutrient retention were traded off against those of inorganic nutrient retention (lower Jaccard's indexes and negative correlations of selection times). Especially, the negative correlation of selection times increased as the conservation target increased from 30% to 50%. The proposed approach provided useful information for assessing the responses of ESs and systematic conservation optimal planning to the land use and climate changes. The systematic conservation optimal areas of hydrological ESs provided an effective trade-off tool between environmental protection (sediment and organic nutrient retentions) and economic development (water yield and inorganic nutrient retention).     

Integrated Economic and Environmental Assessment of Cellulosic Biofuel Production in an Agricultural Watershed

SWAT watershed model simulated biomass yield and pollutant loadings were integrated with associated economic costs of farm production and transport to study two dedicated energy crops, switchgrass and Miscanthus, and corn stover, as feedstocks for a cellulosic biorefinery. A multi-level spatial optimization (MLSOPT) framework was employed to get spatially explicit cropping plans for a watershed under the assumption that the watershed supplies biomass to a hypothetical biorefinery considering both the biochemical and the thermochemical conversion pathways. Consistent with previous studies, the perennial grasses had higher biomass yield than corn stover, with considerably lower sediment, nitrogen, and phosphorus loadings, but their costs were higher. New insights were related to the tradeoffs between cost, feedstock production, and the level and form of environmental quality society faces as it implements the Renewable Fuel Standard. Economically, this involved calculating the farthest distance a biorefinery would be willing to drive to source corn residue before procuring a single unit of perennial grasses from productive agricultural soils.     

聚丙烯酰胺对坡地苹果园水土流失和土壤养分流失的影响

为了改善坡地苹果园的土壤环境,遏制水土流失和土壤养分流失,探寻聚丙烯酰胺适宜的干撒施用量,2010—2012年在陕北丘陵沟壑区的坡地苹果园,以不施聚丙烯酰胺为对照,分别撒施0.6、0.8、1.0、1.2、1.4和1.6 g·m^-2的聚丙烯酰胺,监测果园地表产流、土壤流失、养分流失和苹果植株生长状况.结果表明: 坡地果园的径流量和5—7月的产流次数均随聚丙烯酰胺撒施量的增加呈“V”型变化,其中撒施量为1.0 g·m^-2时最低,但果园侵蚀泥沙量则随聚丙烯酰胺撒施量的增加而降低.地表径流和侵蚀泥沙中的铵态氮、速效磷和速效钾的浓度均随聚丙烯酰胺撒施量的增加而降低;聚丙烯酰胺可显著降低地表径流中的硝态氮含量,对侵蚀泥沙中的硝态氮含量则无显著影响;侵蚀泥沙中的有机质、全氮、全磷和全钾含量均随聚丙烯酰胺撒施量的增加而降低.聚丙烯酰胺提高了苹果单果质量及产量,但对苹果植株生长及果实风味品质无显著影响.聚丙烯酰胺在坡地苹果园中的适宜撒施量应为1.0 g·m^-2.     

Simulation of watershed hydrology and stream water quality under land use and climate change scenarios in Teshio River watershed,northern Japan

Quantitative prediction of environmental impacts of land-use and climate change scenarios in a watershed can serve as a basis for developing sound watershed management schemes. Water quantity and quality are key environmental indicators which are sensitive to various external perturbations. The aim of this study is to evaluate the impacts of land-use and climate changes on water quantity and quality at watershed scale and to understand relationships between hydrologic components and water quality at that scale under different climate and land-use scenarios. We developed an approach for modeling and examining impacts of land-use and climate change scenarios on the water and nutrient cycles. We used an empirical land-use change model (Conversion of Land Use and its Effects, CLUE) and a watershed hydrology and nutrient model (Soil and Water Assessment Tool, SWAT) for the Teshio River watershed in northern Hokkaido, Japan. Predicted future land-use change (from paddy field to farmland) under baseline climate conditions reduced loads of sediment, total nitrogen (N) and total phosphorous (P) from the watershed to the river. This was attributable to higher nutrient uptake by crops and less nutrient mineralization by microbes, reduced nutrient leaching from soil, and lower water yields on farmland. The climate changes (precipitation and temperature) were projected to have greater impact in increasing surface runoff, lateral flow, groundwater discharge and water yield than would land-use change. Surface runoff especially decreased in April and May and increased in March and September with rising temperature. Under the climate change scenarios, the sediment and nutrient loads increased during the snowmelt and rainy seasons, while N and P uptakes by crops increased during the period when fertilizer is normally applied (May through August). The sediment and nutrient loads also increased with increasing winter rainfall because of warming in that season. Organic nutrient mineralization and nutrient leaching increased as well under climate change scenarios. Therefore, we predicted annual water yield, sediment and nutrient loads to increase under climate change scenarios. The sediment and nutrient loads were mainly supplied from agricultural land under land use in each climate change scenario, suggesting that riparian zones and adequate fertilizer management would be a potential mitigation strategy for reducing these negative impacts of land-use and climate changes on water quality. The proposed approach provides a useful source of information for assessing the consequences of hydrology processes and water quality in future land-use and climate change scenarios.     

湖泊底质与水生植物相互作用综述

简要阐述了湖泊生态系统中底质和水生植物的概念及重要性,综述了底质理化性质对水生植物生长的影响,以及水生植物对底质营养盐的释放和底质再悬浮的作用。通过大量的研究综述回顾论述了不同的湖泊底质类型在一定程度上决定了水生植物的生长状态,适合的底质营养盐范围能促进水生植物生长,不同水生植物对底质营养盐的耐受性有差异。水生植物能促进底质沉降并减少再悬浮,水生植物的存在对沉积物中磷的活性有显著的影响。污染底泥的修复能为水生植物的立地与生长提供了良好的底质条件,有利于富营养化湖泊水生植被的恢复与重建。     

黄土高原典型退耕区生态系统服务权衡与协同关系研究——以延安市为例

在退耕还林的背景下,从多尺度分析黄土高原生态系统服务的时空变化及权衡协同关系对促进该区经济发展和生态效益多赢具有重要意义。以黄土高原退耕还林典型区延安市为例,运用InVEST模型评估1988-2018年农作物生产、碳储量、生境质量、土壤保持、产水量5种关键生态系统服务物质量,采用偏相关分析法探讨生态系统服务间的权衡与协同关系及其时空变化特征。研究结果表明：（1）受土地利用变化影响,延安市农作物生产水平、土壤保持年际变化趋势波动较大,农作物生产水平呈波动增加的趋势,土壤保持退耕还林前呈减少,退耕还林后呈波动增加的趋势,碳储量和生境质量呈逐渐增加的趋势,产水量呈逐渐减弱的趋势。（2）生态系统服务与土地利用格局联系紧密。碳储量、生境质量的高值区域以及产水量的低值区域随林地分布格局变化而变化。（3）协同关系是延安市生态系统服务间相关关系的主体,主要发生在碳储量、生境质量、土壤保持、农作物生产之间,权衡关系主要存在于产水量和其他生态系统服务之间。（4）市、县域生态系统服务间关系的差异主要发生在生境质量和土壤保持之间。