Ecological Restoration and Landscape Construction of Wetland——A Case Study of Planning and Design of Mi River Wetland Park in Linqu of Shandong

Based on geological characteristic of Mi River Wetland Park in Linqu of Shandong,the paper had illustrated historical and cultural spirits of Linqu,and then proposed planning strategies and contents of Mi River Wetland Park.It discussed new approaches for wetland restoration and landscape construction from the perspectives of ecological restoration of wetland system,overall construction of leisure system,and full display of regional characteristic.The construction of wetland system laid stress on water system design,terrain treatment,vegetation construction,and biological diversity creation.Wetland system would be overlaid with leisure system,divided into wetland leisure zone,wetland entertainment zone,humanity landscape zone,wetland science popular zone and wetland experience zone,all of which would be constructed with characteristic respectively.On the basis of site character,the paper had searched an energy balance and substance transformation method between rivers,plants,earth and humans,of certain practicality.

Ecological Environment Problems and Countermeasures of Small and Middle-sized Rivers in Shandong Province

Water uses in small and middle-sized rivers, and non-ecological treatment model has deteriorated local environment in Shandong. The research reviewed ecological environment status quo of small and middle rivers and concluded existing problems. Finally, ecological treatments were proposed based on treatments at home and abroad in order to improve eco-environment of rivers and build better Shandong.

A PRELIMINARY STUDY OF THE YELLOW RIVER'S PALEOCHANNELS IN NORTH SHANDONG PLAIN

According to buried depth, the Yellow Rver's Paleochannels can be divided into ground Paleochannels (buried depth 0-8m) and shallowburied Paleochannels theried depth 8-50m). Each of them can be roughly divided into three major Paleochannel belts, stretching Parallel with each other from SW to NE. Sedimentary layers of the paleochannels were mainly made up by sand levee of meanders or natural leavee deposits, and the flooding sedments were found bebeen the layers. The paleochannels in North Shadong Plain were formed in three stags; stage I (buried depth 50-15m) in later period of late Pleistocene-early period of Holocene, stag II (20-8m) in earlymiddle period of HOlocene; and stag III (8-0m) in midddle-late period of Holocene.

Environmental change and cultural response around 4200 cal. yr BP in the Yishu River Basin, Shandong

Neolithic culture series in the Yishu River Basin developed in the order of Beixin culture-Dawenkou culture-Longshan culture-Yueshi culture. During the early and middle stage of Longshan culture （4600-4300 cal. yr BP）, the climate in the Yishu River Basin was warm and wet. Paddy-oriented agriculture planted paddy was very developed. The society was flourishing with great amount of archaeological sites. The cooling starting in 4200 cal. yr BP made the paddies shortfall in output or even no seeds were gathered. This situation intensified the discrepancy between population and resource. The scarcity in natural resource led to substantial decrease in population and subsequent drop in archaeological sites. About 4000 cal. yr BP Longshan culture was displaced by Yueshi culture which was relatively un- derdeveloped, simple and unsophisticated.

A STUDY ON THE WATER RESOURCES AND SEDIMENT PROBLEMS IN THE IRRIGATED AREA OF NORTHWEST SHANDONG PROVINCE

There are very serious water and sediment problems in the irrigated areas of northwest Shandong Province. In upper reaches of the irrigated area, the Yellow River water are widely used for farmland watering while leaving the ground water unusedion. But in the lower reaches, there is not enough surface water to be channeled for irrigation, so the ground water has always been over extracted, in some parts of the lower reaches, the descending water table caused the formation of funnel. Siltation in canals are very difficult to be cleared up, the drop of agriculture yield in the sandy land close to the channel head and along the main channels impair the living conditions of the local people. The conflicts between the excessive dependence on the Yellow River and the decreasing tendancy of water amount provided by the Yellow Ricer forces the local government to find new ways to solve the water resource problems. The answer could be: Using new technique for the irrigated system, pay more attention to the ground water development, and the construction and maintenance of wells.

Sedimentary Evolution of the Holocene Subaqueous Clinoform off the Southern Shandong Peninsula in the Western South Yellow Sea

Based on the stratigraphic sequence formed since the last glaciation and revealed by 3000 km long high-resolution shallow seismic profiles and the core QDZ03 acquired recently off the southern Shandong Peninsula, we addressed the sedimentary characteristics of a Holocene subaqueous clinoform in this paper. Integrated analyses were made on the core QDZ03, including sedimentary facies, sediment grain sizes, clay minerals, geochemistry, micro paleontology, and AMS 14 C dating. The result indicates that there exists a Holocene subaqueous clinoform, whose bottom boundary generally lies at 15–40 m below the present sea level with its depth contours roughly parallel to the coast and getting deeper seawards. The maximum thickness of the clinoform is up to 22.5 m on the coast side, and the thickness contours generally spread in a banded way along the coastline and becomes thinner towards the sea. At the mouths of some bays along the coast, the clinoform stretches in the shape of a fan and its thickness is evidently larger than that of the surrounding sediments. This clinoform came into being in the early Holocene(about 11.2 cal kyr BP) and can be divided into the lower and upper depositional units(DU 2 and DU 1, respectively). The unit DU 2, being usually less than 3 m in thickness and formed under a low sedimentation rate, is located between the bottom boundary and the Holocene maximum flooding surface(MFS), and represents the sediment of a post-glacial transgressive systems tract; whereas the unit DU 1, the main body of the clinoform, sits on the MFS, belonging to the sediment of a highstand systems tract from middle Holocene(about 7–6 cal kyr BP) to the present. The provenance of the clinoform differs from that of the typical sediments of the Yellow River and can be considered as the results of the joint contribution from both the Yellow River and the proximal coastal sediments of the Shandong Peninsula, as evidenced by the sediment geochemistry of the core. As is controlled mainly by coactions of multiple factors such as the Holocene sea-level changes, sediment supplies and coastal dynamic conditions, the development of the clinoform is genetically related with the synchronous clinoform or subaqueous deltas around the northeastern Shandong Peninsula and in the northern South Yellow Sea in the spatial distribution and sediment provenance, as previously reported, with all of them being formed from the initial stage of the Holocene up to the present.

Temporal and spatial evolution of surface sediments characteristics in the Dagu River estuary and their dynamic response mechanism

Based on the 39 surface sediment samples collected in the flood season and the dry season in 2012 respectively and the measured hydrological data in October 2012, the sediment grain size characteristics has been analyzed and the response mechanism of surface sediments to estuarine hydrodynamics was revealed by calculating the range of waves and tidal currents. The results show that:(1) The grain size of the surface sediment samples decreased gradually from land to sea in the flood season. The fine sediment was redistributed under marine hydrodynamics in the dry season and the sediments showed coarser tendency ingeneral;(2) tidal current stirring sediment was very obvious in Dagu River estuary area, and wave stirring sediments mainly occurred in the tidal flat area and estuary sand bar area;(3) in the flood season, surface sediment sat the estuary were transported towards south and southeast. In the dry season, surface sediments were transported towards southwest at the north area of Jiaozhou Bay Bridge, and sediments were transported towards northeast area at the south of Jiaozhou Bay Bridge.

黄河流域(山东段)工业用地错配时空格局与应对策略

以黄河流域(山东段)9个设区市所辖77个区县为研究单元,利用2011—2020年山东省供地信息库中的工业用地供应数据,以及同期工业经济统计数据,分析黄河流域(山东段)工业用地供应与工业利润总额时空变化特征,通过空间错配指数分析工业用地错配时空格局,并从科学配置、存量挖潜、提质增效和层级协同4个方面提出应对策略。研究对于实现黄河流域(山东段)土地资源高效利用与聚集区域高质量发展具有重要意义。

黄河流域山东段国土空间格局演变及驱动因素研究

以黄河流域山东段为研究区,结合2000—2020年土地利用数据和社会经济统计数据,从规模特征、动态变化和分布特征等方面对国土空间时空演变格局进行多维度定量分析,并采用地理探测器探析其驱动因素。结果表明:(1)规模特征方面,除乡村生活空间规模相对稳定外,其他各类国土空间增减特征显著;(2)动态变化方面,不同国土空间类型间的动态变化差异明显,且各区县单元综合动态度呈现东北高、西南低、中部突出的特征;(3)分布特征方面,各国土空间面积变化具有显著的空间集聚特征,这一特征在2010—2020年相对减弱;(4)驱动因素方面,研究区国土空间面积变化受到地形地貌、水热状况、区位情况以及社会经济等多种因素的共同影响,自然环境因素是国土空间格局演变的重要地理基础,社会经济发展则发挥着关键的推动作用。

黄河流域(山东段)村镇聚落文化景观基因识别指标体系构建

黄河流域(山东段)村镇聚落孕育了丰富独特的文化景观,建立识别指标体系对其文化景观基因进行挖掘整理,对在黄河流域生态保护和高质量发展战略背景下赓续传统文化具有重要意义。结合景观基因理论的研究成果和对国家有关政策法规文件的剖析,在历史景观视角下对黄河流域(山东段)的村镇聚落开展深入的文化景观田野调查、典籍研究等,提出具有针对性的文化景观基因识别指标体系构建逻辑,通过“识别对象—识别因子—识别指标”解析出13项识别因子、40项识别指标,为黄河流域村镇聚落文化景观识别全覆盖提供新的思路与方法。

山东省黄河三角洲水生耐盐药用植物资源调查与分析

对山东省黄河三角洲地区水生耐盐药用植物的种类、生活型及对应药材入药部位、药性、功效进行统计调查分析。共调查到野生水生耐盐药用植物299种。根据恩格勒分类系统,这些植物隶属于76科204属;生活型以草本型为主,共222种。以299种药用植物为基源的药材共338种,其中全草入药药材144种,占药材种类数的42.60%;平性药材最多,共85种;苦味药、甘味药和辛味药数量较其他药味具有明显优势;以功效分类,清热药、利水渗湿类、活血化瘀类、化痰止咳类、止血药和补虚药占优势。针对水生耐盐药用植物特点,结合该区域自然状况,提出了合理开发和综合利用的建议。

基于灰色关联模型的沿黄区域山东段生态安全综合评价及时空演化

以沿黄区域山东段为例,建立PSR模型构建生态安全评价指标体系,借助熵权法和灰色关联度模型对其2000—2018年展开生态安全综合评价,并进行时空演变分析。结果显示,整体上沿黄区域山东段生态安全水平呈现出波动中上升的趋势,由“不安全”向“比较安全”转变,子系统中生态响应和生态状态增加的幅度高于生态环境压力增大的幅度,生态环境有所好转;市级尺度下,山东段17地市生态安全水平有所提高,呈现出“下降-上升-下降”的倒“N”字形演变,生态安全类型以“一般安全”为主,高等级类型较少,城市生态安全问题比较严峻;城市生态安全内部空间差异明显,生态安全空间格局向东、向北转移,呈现出“东高西低”“北高南低”的高低错落分布,高等级生态安全区域从东部沿海向鲁北扩散,“临界安全”区域缩小至鲁中南和鲁西北。最后从生态环境治理与保护、优化调控三大空间、经济结构转型升级等方面提出优化路径,改善生态环境质量。

山东省黄河流域红色体育文化资源的开发与利用

培育发展红色体育文化资源,构建中国特色的红色体育文化产业,是中国红色文化继承与发扬的重要课题。山东省黄河流域拥有历史悠久的文化底蕴和丰富的红色体育文化资源。山东省推出红色文化旅游、红色体育文化活动、红色体育场馆建设等举措,有效激活了红色体育文化的生命力;然而,在保护与传承、开发、运营、宣传方面仍存在不足。可以考虑从加强保护、创造性开发、提高运营战略、拓展宣传渠道等多个层面积极推进其在当下的价值实现。

场域理论视域下山东黄河档案编研工作探究

黄河档案编研工作是追溯黄河历史、弘扬黄河精神的重要途径。为响应国家黄河战略,探究黄河档案编研工作提质增效的发展向路,文章基于对山东黄河档案编研现状的调研分析,以布尔迪厄场域理论为研究坐标,把握山东黄河档案场域内部运行机制,剖析编研工作主要行动者在资本和惯习上的缺位,从内部资本培育、外部资本吸纳和内外惯习平衡三个方面提出山东黄河档案编研工作的未来走向,通过战略性和系统性思维促进档案开发利用工作的科学化和现代化。

黄河流域典型县域生境质量的时空分异特征及影响因素研究

通过探索黄河流域山东段县域生境质量时空分异特征与影响因素,以便从县域尺度为地方生态环境保护与社会经济高质量发展提供政策建议。基于2000、2010和2020年3期土地利用数据,采用InVEST模型解析生境质量的时空分布格局与演变特征,结合空间自相关模型对其空间分异特征进行探测,并采用地理加权回归(GWR)模型分析社会、经济与自然影响因素在空间维度上对生境质量的影响。结果表明:(1)2000—2020年,黄河流域山东段平均生境质量指数为0.448,空间上表现出中段、上段低和下段高的分布格局,生境质量整体呈先快速下降后缓慢下降趋势,中段生境质量下降趋势最为显著;(2)生境质量变化在空间分布上呈显著集聚性特征,会受到邻近区域的影响,且总体集聚态势不断增强,高-高型集聚区面积明显大于低-低型集聚区,在流域下段范围连片分布;(3)土地开发强度是影响生境质量时空分布的首要因素,城市化水平、人口密度和NDVI对生境质量有重要影响,社会、经济和自然因素共同影响生境质量时空变化,GWR回归分析结果表明生境质量具有空间差异性。识别这些时空差异对推动该区域生态高质量发展具有重要意义。

淮河流域及山东半岛地下水超采原因与管理对策

针对淮河流域及山东半岛地区地下水严重超采的问题,从地下水开发利用趋势、水位动态变化、生态与环境地质问题等方面分析了该地区地下水超采的状况,从水资源禀赋条件、水资源承载能力、城镇用水需求变化、地下水监管能力等方面剖析了地下水超采的原因。针对地下水双控指标体系、监测计量、信息化监管等方面存在的问题,从强化流域对地下水资源统一管理的角度提出了相关对策建议。

基于DEA模型的山东省沿黄流域果业生产效率提升研究

沿黄流域果业高质量发展对落实黄河流域生态保护和高质量发展国家战略,推动果业振兴、乡村振兴意义重大。综述了果业生产效率相关研究,基于实际调研了山东省菏泽、滨州、东营市的果园情况和数据,构建了山东省沿黄流域果品投入产出指标体系,利用DEA模型进行果业生产效率测算,有针对性地提出发展规模经营、调整投入结构比例、强化现代栽培管理、发展智慧化生产等建议,以期推动沿黄流域果业高质量发展。

山东省沿黄地区规模化牛场全株玉米青贮发酵品质及营养价值评价

为了评定山东省沿黄地区全株玉米青贮发酵品质和营养价值,以了解规模化牛场青贮玉米的制作现状,试验于2023年3—5月份分别采集沿黄地区滨州市、东营市、德州市、菏泽市、济宁市、济南市、聊城市、泰安市、淄博市的规模化奶牛场(51个)和肉牛场(54个)全株玉米青贮饲料样品共105份,测定样品的发酵品质和营养成分,参照《青贮玉米品质分级》(GB/T 25882—2010)对全株玉米青贮品质进行分级。结果表明:淄博市全株玉米青贮中乳酸含量显著高于其他市(P<0.05);德州市全株玉米青贮pH值显著高于滨州市、东营市、菏泽市、聊城市、泰安市和淄博市(P<0.05),其中淄博市全株玉米青贮pH值最低(3.15)。泰安市、滨州市全株玉米青贮淀粉含量较高,极显著高于东营市、德州市、菏泽市、济宁市、淄博市(P<0.01),聊城市极显著高于德州市、济宁市(P<0.01);济南市显著高于德州市、济宁市(P<0.05)。济南市全株玉米青贮中性洗涤纤维含量最高,极显著高于菏泽市、济宁市,滨州市、聊城市极显著高于济宁市(P<0.01)。德州市全株玉米青贮酸性洗涤木质素含量最高,极显著高于滨州市、东营市、聊城市、泰安市、淄博市(P<0.01),显著高于济南市(P<0.05);菏泽市、济宁市极显著高于淄博市(P<0.01)。德州市全株玉米青贮粗灰分含量最高,显著高于滨州市、东营市、聊城市、淄博市(P<0.05),菏泽市显著高于滨州市、聊城市、淄博市(P<0.05)。泰安市、济南市、滨州市、聊城市全株玉米青贮粗脂肪含量较高,极显著高于济宁市(P<0.01);东营市、德州市、淄博市显著高于济宁市(P<0.05)。各市间全株玉米青贮中乙酸、丙酸、酸性洗涤纤维、干物质、粗蛋白含量均差异不显著(P>0.05)。泰安市全株玉米青贮饲料品质为一级;济南市、聊城市、滨州市为二级;淄博市、济宁市、德州市、东营市和菏泽市为三级。说明沿黄地区全株玉米青贮饲料品质良好。

鲁西南黄河下游地下水氟富集规律及其影响因素

鲁西南平原位于黄河下游,现阶段对该区地下水水化学成因及其对地下水中F元素富集影响机理的研究较少。该研究以鲁西南平原沿黄河地带地下水为主要研究对象,采集浅层地下水样品36件,深层地下水样品16件,黄河水样品2件进行全分析测试;通过统计、相关性分析、水化学模拟等方法手段,计算氯碱指数(CAI),绘制Durov图、Gibbs图、Ca^(2+)/Na^(+)–Mg^(2+)/Na^(+)图、log_(10)(Ca^(2+))_(activity)–log_(10)(F^(-))_(activity)图等图件,分析了研究区地下水水化学成因及其富氟机理。结果显示,鲁西南沿黄区浅层及深层地下水化学类型均以HCO_(3)-Na为主,整体偏碱性,地下水氟含量分别为1.59 mg/L、2.35 mg/L,深层水氟含量水平变化程度低于浅层;区内浅层地下水氟与Ca^(2+)含量呈显著负相关,与pH值呈显著正相关,深层地下水中氟与Na^(+)、TDS值呈显著正相关。鲁西南沿黄区地下水氟含量主要来源于萤石(Ca F_(2))的溶解,受水岩作用和阳离子交换作用共同控制下的Ca^(2+)含量制约。此研究揭示了黄河下游主要地下水含水层中氟富集规律和影响因素。

鲁西南黄泛区耕地格局变化特征及其影响因素

[目的]探讨鲁西南黄泛区耕地的空间格局、变化特点及其影响因素,为区域耕地保护提供科学依据。[方法]基于2m高分遥感影像,结合野外调查和《菏泽市统计年鉴》,采用遥感解译、重心模型、冷热点分析、地理探测器等方法,分析2019—2022年鲁西南黄泛区耕地空间分布、重心迁移、年际变化特征及影响因素。[结果](1)2019—2022年鲁西南黄泛区耕地面积占区域60%以上,每年均存在耕地流失现象,流失面积呈现逐年递减趋势,郓城县耕地面积减少最多,达18.28 km^(2),鄄城耕地动态度变化最大,达-2.26%;耕地重心整体向东北方向迁移。(2)耕地流出面积高于流入面积,主要流出方向和流入方向均为建设用地和林地,耕地变动最集中的区域主要分布在曹县南部。(3)对耕地变化影响最强的单因子是农村从业人员(X_(5)),最强的双因子交互组合是农村劳动力资源数(X_(4))和城镇居民人均收入(X_(6))。[结论]鲁西南黄泛区2019—2022年耕地流失是经济社会因子为主的多因子综合作用的结果。