塔里木河干流中游灌区退耕封育效益分析

塔里木河干流中游灌区退耕封育的规模为 9× 10 3 hm2 ,其中 ,库灌区退耕 1.4 2× 10 3 hm2 ,河灌区退耕 3.5 7× 10 3 hm2 ,泵灌区退耕 4 .0 1× 10 3 hm2 。退耕封育后 ,农田灌溉用水改为生态灌溉用水 ,用水量减少。人工种植的农作物被天然野生植被所替代 ,同时可提高对保留耕地的利用率 ,扩大耕地的播种面积 ,增加地表植被的覆盖度。退耕封育后 ,可节约水量 0 .97× 10 8m3 ,除满足封育生态用水外 ,还可增加塔里木河下泄水量 0 .31× 10 8m3 。     

施磷和接种根瘤菌对黄河三角洲紫花苜蓿生长及品质的影响

田间试验研究了施磷肥和接种根瘤菌对黄河三角洲地区紫花苜蓿生长及品质的影响.结果表明,播种前施磷肥能明显提高紫花苜蓿的出苗和成苗率,显著提高紫花苜蓿的叶茎比、叶面积指数、叶绿素含量,并提高干物质产量12.9%～85.5%.施磷肥还显著提高了紫花苜蓿地上部可溶性碳水化合物和粗蛋白质的含量,降低了中性洗涤纤维含量,使饲草体外干物质消化率增加0.73%～8.49%.播种时接种根瘤菌能显著增加紫花苜蓿单株根瘤结瘤数和平均根瘤重,并能改善苗期的生长,但对干物质产量影响不明显.试验结果显示,黄河三角洲地区种植紫花苜蓿施用过磷酸钙750 kg/hm2,并接种根瘤菌可获得较好的提高产量和改善品质的效果.     

三江源区高寒草原土壤湿度变化特征及与气候因子的关系

利用青海省三江源区兴海县牧业气象站1999-2016年高寒草原土壤湿度、牧草生育期资料,分析了高寒草原土壤湿度的年、季变化特征以及牧草生长季不同生育期土壤湿度的变化特征及与气候因子的关系。结果表明:高寒草原0-10、10-20、20-30、30-40和40-50 cm土壤湿度均随年际延长呈增加趋势,春季除40-50 cm土层外,其他各层土壤湿度均随年际延长呈显著增加趋势(P<0.05)。高寒草原牧草生长季的土壤相对湿度随年际延长呈显著上升趋势(P<0.05),且与生长季降水量之间呈极显著正相关关系(P<0.01)。随着气候变化,牧草抽穗、开花、成熟和枯黄期的土壤相对湿度随年际延长呈显著增加趋势(P<0.05)。牧草抽穗期、枯黄和全生育期的土壤湿度与气温呈显著负相关关系(P<0.05)。高寒草原牧草生长季土壤湿度的增加有利于草地植被生长。     

河南长江流域防护林工程水土保持效益评价

涵养水源和保育土壤是森林的主要生态功能。通过采用森林生态系统服务功能实物量、价值量评估方法对长防林工程实施区域森林的水土保持效益进行的评价,结果表明,长防林工程实施后林地可调节水量12.936亿m3,固土0.135亿t,林地的水土保持效益价值达126.247亿元。经过20年的长防林工程建设,项目区内森林资源快速增长,水土流失面积大幅度减少,工程建设对生态环境的改善起到了明显的作用。     

河南卫河流域脆弱性评价

结合卫河自身特点和地理环境建立13项指标体系,运用基于熵权的模糊数学模型对其脆弱性进行评价。结果表明,鹤壁的脆弱性为0.69,焦作为0.55,新乡为0.39,安阳为0.36,濮阳为0.23。最后针对评价结果分析了原因,提出了合理性建议和措施。     

保定市一亩泉河河流中COD的变化及污染源分析

针对保定市城区水系管理委员会2017年3月公布的黑臭水体河流中的一亩泉河7.23km的黑臭水体段为参考进行了勘查、取样与COD实验工作,从2019年4月12日到2019年5月29日进行了为期一个半月的时间。研究结果表明:保定市一亩泉河河流不同位置COD大小不同、污染原因不同。通过周围景观的变化、对采样点附近居民进行的走访和COD浓度的测定,对一亩泉河的水质状况和污染源进行了全面系统地分析。并为此提出了切实可行、经济有效、便于管理的控制方案。     

甘肃黄河三峡景区旅游资源空间结构研究

旅游空间结构是旅游系统功能组织方式在空间上的投影或表象,其空间结构是否合理直接影响到旅游目的地旅游业的发展态势。黄河三峡景区凭借其丰富、独特的资源优势,已成为黄河流域最著名的景区之一。受河谷地带的基础性影响,其资源类型、空间结构、游览线路等表现出典型的空间特征,深刻影响着景区旅游空间格局。借助Arc GIS空间网络分析模块和Excel平台,对黄河三峡景区旅游资源空间结构进行定量分析,发现旅游资源空间分布呈集聚态势,基尼系数高达0.755,分布均匀度仅为0.245;采用最邻近指数和Voronoi多边形的变异系数分析空间分布类型;用地理集中指数和基尼系数分析空间分布均衡性,运用β指数、γ指数和α指数刻画空间连接度。结果表明:景区内旅游资源的空间分布均匀度低,呈多中心集聚分布。这既有利于景区内各景点之间的整合和旅游规模效应的产生,又可以减弱区间屏蔽作用等外部不经济性。景区内各景点之间的交通网络密度低,空间联系较弱,通达性较低。各景点之间的直接连接较少,旅游路线多为单线往返,缺少串联各个景点的环形线路。     

西双版纳南览河流域常见观赏蝶种及其寄主植物资源调查

西双版纳勐海县境内南览河流域具有良好的天然植被,蝴蝶种类繁多。为了开展重要观赏蝶种的人工繁育试验,2013—2018年对南览河中低海拔地带的常见观赏蝴蝶及其野生寄主植物资源开展了进一步的深入调查,结果表明,经过5年定点调查和沿线观察,在区域内发现兼具较高观赏价值及人工繁育潜力的蝶种46个;通过观察野外成虫的产卵活动,结合野外套袋及室内饲养幼虫,发现蝴蝶寄主植物38种,初步查明了相关蝶种的野生寄主植物资源。调查工作可为筛选出当地适生优良寄主植物、进一步开展相关蝶种的人工养殖试验提供参考。     

Influence of salinity and moisture on the threshold shear velocity of saline sand in the Qarhan Desert,Qaidam Basin of China: A wind tunnel experiment

Determination of the threshold shear velocity is essential for predicting sand transport, dust release and desertification. In this study, a wind tunnel experiment was conducted to evaluate the influence of salinity and moisture on the threshold shear velocity of saline sand. Saline sand samples (mean particle size of 164.50-186.08 μm and the total silt, clay and salt content of 0.80%-8.25%) were collected from three saline sand dunes (one barchan dune and two linear dunes) in the Qarhan Desert, Qaidam Basin of China. Original saline sand samples were placed in two experimental trays for wet and dry processing to simulate deliquescence and desiccation, respectively. Surface moisture content ranging from 0.30% to 1.90% was generated by the steam method so that the saline sand can absorb water in a saturated water vapor environment. The motion of sand particles was determined by the observers with a solid laser. The laser sheet (0.80 cm thick), which was emitted by the solid laser, horizontally covered the sand surface and was bound to the sand. Results show that the cohesion of saline sand results from a combination of salt and water. The threshold shear velocity increases exponentially with the increase in crust thickness for the linear sand dunes. There is a positive linear correlation between the original moisture content and relative threshold shear velocity. The threshold shear velocity of dewatered sand is greater than that of wet sand with the same original moisture content. Our results will provide valuable information about the sand transport of highly saline soil in the desert.     

Influences of sand cover on erosion processes of loess slopes based on rainfall simulation experiments

Aeolian-fluvial interplay erosion regions are subject to intense soil erosion and are of particular concern in loess areas of northwestern China.Understanding the composition,distribution,and transport processes of eroded sediments in these regions is of considerable scientific significance for controlling soil erosion.In this study,based on laboratory rainfall simulation experiments,we analyzed rainfall-induced erosion processes on sand-covered loess slopes(SS)with different sand cover patterns(including length and thickness)and uncovered loess slopes(LS)to investigate the influences of sand cover on erosion processes of loess slopes in case regions of aeolian-fluvial erosion.The grain-size curves of eroded sediments were fitted using the Weibull function.Compositions of eroded sediments under different sand cover patterns and rainfall intensities were analyzed to explore sediment transport modes of SS.The influences of sand cover amount and pattern on erosion processes of loess slopes were also discussed.The results show that sand cover on loess slopes influences the proportion of loess erosion and that the compositions of eroded sediments vary between SS and LS.Sand cover on loess slopes transforms silt erosion into sand erosion by reducing splash erosion and changing the rainfall-induced erosion processes.The percentage of eroded sand from SS in the early stage of runoff and sediment generation is always higher than that in the late stage.Sand cover on loess slopes aggravates loess erosion,not only by adding sand as additional eroded sediments but also by increasing the amount of eroded loess,compared with the loess slopes without sand cover.The influence of sand cover pattern on runoff yield and the amount of eroded sediments is larger than that of sand cover amount.Furthermore,given the same sand cover pattern,a thicker sand cover could increase sand erosion while a thinner sand cover could aggravate loess erosion.This difference explains the existence of intense erosion on slopes that are thinly covered with sand in regions where aeolian erosion and fluvial erosion interact.