北京市昌平区统筹城乡区域发展研究

北京市昌平区通过大力实施乡村振兴战略,深入推进城乡区域协调发展,在城乡基本公共服务发展、产业发展、乡村治理、人才队伍建设等方面取得了一定进展.但同时也存在产业发展缓慢、人才力量不足等问题,为此,提出推动城乡基本公共服务均衡发展,多措并举加快乡村产业发展,创新和完善乡村治理机制,促进实用人才培养等四个方面的建议.     

振安区农机深松整地作业技术推广应用研究

实施农机深松整地作业技术有利于农业可持续发展。介绍振安区农机深松整地技术发展现状与技术模式,阐述该技术推广应用中采取的措施及存在的问题,提出逐步建立起技术示范应用长效机制,以期为科学高效地推进农机深松整地技术在振安区的推广应用提供参考。     

不同施氮水平对柳枝稷光合特性及抗旱性的影响

为了探究宁夏银北盐碱地区柳枝稷高产优质高效栽培过程中最佳的施氮量及其对柳枝稷叶片光合特性及抗旱性的影响,本研究采用大田试验,以Cave-in-Rock品种柳枝稷为供试材料,设无氮添加(0 kg·hm-2,N0)、施低氮(60 kg·hm-2,N60)、中氮(120 kg·hm-2,N120)和高氮(240 kg·hm-2,N240)共4个施氮水平,分析比较了各生育时期内柳枝稷叶片光合特性、渗透调节物质及抗氧化酶活性的变化,同时采用隶属函数法综合评价了盐碱地柳枝稷的抗旱性.结果表明,随着不同施氮水平的增加,柳枝稷各生育时期内叶片叶绿素相对含量(SPAD)、净光合速率(Pn)、气孔导度(Gs)和细胞间隙CO2浓度(Ci)整体呈现先升后降的趋势,均在施中氮(N120)处理下达到峰值.与无氮添加(N0)处理相比,施低氮(N60)、中氮(N120)和高氮(N240)处理下柳枝稷叶片的SPAD值平均增加了4.73％、18.71％和8.86％,净光合速率(Pn)平均提高了5.55％、17.02％和12.41％,气孔导度(Gs)平均升高了7.87％、56.18％和39.33％,细胞间隙CO2浓度(Ci)平均增加了7.86％、30.71％和13.81％.柳枝稷叶片蒸腾速率(Tr)在高氮(N240)处理下达到最大值,叶片水分利用效率(WUE)随着不同施氮水平的增加而逐渐下降.隶属函数分析结果表明,施中氮(N120)处理下柳枝稷各抗旱指标隶属函数值的均值最大.因此,本试验条件下有利于提高柳枝稷叶片光合能力和抗旱性的适宜施氮水平为120 kg·hm-2.     

中国蔬菜产业发展中化肥和农药使用问题的思考

针对蔬菜中化肥和农药过量施用产生的重大问题,该文做了客观分析和思考,并提出了相应的对策,以期为降低化肥和农药的用量,落实“双减”战略提供参考。     

Investigation of environmental and land use impacts in forested permafrost headwaters of the Selenga-Baikal river system,Mongolia - Effects on discharge,water quality and macroinvertebrate diversity

Headwater streams play a major role for provision of ecosystem services, e.g. drinking water. We investigated a high-altitude headwater catchment of the Kharaa River (including 41 1st-order rivers) to understand the impact of land cover (especially forest cover), environment and human usage on runoff, chemical water quality and macroinvertebrate fauna in a river basin under discontinuous permafrost conditions in an arid, sparsely populated region of Mongolia. To verify our hypotheses that different landuses and environmental impacts in permafrost headwaters influence water quality, we investigated 105 sampling sites, 37 of them at intermittent stream sections without water flow. Discharge was positively impacted by land cover types steppe, grassland and forest and negatively by shrubland, forest burnt by wild fires (indicating a reduction of permafrost) and slope. Water quality was affected by altitude, longitude and latitude, shrub growth and water temperature. Shannon diversity of macroinvertebrates was driven by water temperature, iron content of the water, flow velocity, and subbasin size (adjusted R² = 0.54). Sample plots clustered in three groups that differed in water chemistry, macroinvertebrate diversity, species composition and bio-indicators. Our study confirms that steppes and grasslands have a higher contribution to runoff than forests, forest cover has a positive impact on water quality, and diversity of macroinvertebrates is higher in sites with less nutrients and pollutants. The excellent ecological status of the upper reaches of the Kharaa is severely threatened by forest fires and human-induced climate change and urgently needs to be conserved.     

五指山耕地土壤养分现状调查与评价

为了明确海南山区耕地土壤养分空间分布特征，为热带山区耕地土壤养分管理提供思路。以海南五指山市耕地为研究对象，采用野外调查、采样和室内分析相结合的方法，阐述土壤养分现状，探讨其土壤养分分布规律。结果表明：五指山耕地土壤总体呈酸性，其pH值为5.1；土壤有机质、有效磷、速效钾和中量元素(钙、镁、硫)含量均为中等或偏下水平，土壤有效铜和有效锌含量较为丰富。五指山耕地土壤酸化和养分含量分布不均主要与气候、母质分布和施肥不平衡有关。     

Soil protection for a sustainable future: options for a soil monitoring network for Ireland

The increased recognition of the importance of soil is reflected in the UN Post‐2015 Development Agenda with sustainable development goals that directly and indirectly relate to soil quality and protection. Despite a lack of legally binding legislation for soil protection, the European Commission remains committed to the objective of soil protection. However, the achievement of a legally binding framework for soil protection relies on the implementation of a soil monitoring network (SMN) that can detect changes to soil quality over time. As beneficiaries do not pay for the provision of soil information, the options for soil monitoring are limited. The use of existing data sets should be considered first. Using Ireland as an example, this research explored the opportunities for a SMN for Ireland considering three existing national data sets. The options for a SMN are considered in terms of their spatial and stratified distribution, the parameters to be measured and an economic analysis of the options proposed. This research finds that for Ireland, either a 10 or a 16 km² grid interval stratified by land use and drainage class offers the best potential in relation to the spatial distribution of existing data sets to reflect local data at a national level. With existing data, the stratified SIS data using the 16 km² grid offers the best value for money, with baseline costs for analysis, excluding field costs, of between €706 481 and €2.8 million. Acknowledging the impossibility of measuring all parameters with ideal frequency, this study proposes a two‐tier system for optimized monitoring frequency. Parameters must anticipate future policy requirements. Finally, the implementation of a SMN must be accompanied by standardized methods, defined thresholds and action mandates to maintain soil quality within allowable limits.     

青藏高原草地降水利用效率时空动态及对气候变化的响应

本研究利用CASA(Carnegie-Ames-Stanford Approach)模型模拟了2000—2013年青藏高原草地净植被生产力(Net Primary Production，NPP)，结合实测数据、气象数据和土地覆被数据计算了草地降水利用效率（PUE），探究其时空分布特征，以及不同草地类型PUE及其对气候变化的响应。结果表明：青藏高原草地PUE在研究年限内呈现波动增加趋势，增加速率为每年0.0035 g·m^-2·mm^-1，14 a的平均值为0.38 g·m^-2·mm^-1。PUE的空间分布具有明显的异质性，呈现东部高、中西部低的基本格局。PUE分布在0.2～0.4 g·m^-2·mm^-1之间的比例最大，占青藏高原总面积的55.63%，呈减少趋势的区域主要分布在青藏高原的北部和西部，以及东部的边界地区，呈增加趋势的地区集中在研究区的中部和南部。研究年限内PUE的变异系数分布在0.07～0.85之间，变化稳定的区域所占面积最大，为总面积的43.43%，主要分布在唐古拉山脉和横断山脉附近。不同草地类型间PUE均值存在差异，具体表现为：草甸（1.06 g·m^-2·mm^-1）>坡面草地（0.80 g·m^-2·mm^-1）>平原草地（0.30 g·m^-2·mm^-1）>高山与亚高山草甸（0.29 g·m^-2·mm^-1）>荒漠草地（0.23 g·m^-2·mm^-1）>高山与亚高山草地（0.094 g·m^-2·mm^-1）。总体上，青藏高原草地PUE与降水成负相关关系，而与气温呈正相关，PUE的变化对降水响应更加敏感。     

金安区农药安全使用调查

安全、合理使用农药是农业生产的重要环节,也对农业生态环境和农民的身体健康有着重要影响。通过对六安市金安区农药安全使用的调查,总结了普遍存在的问题。今后植保部门应加强示范、宣传、指导、培训工作,同时大力推广农作物病虫害专业化防治模式,保障农业健康发展,保护农村生态环境。     

长武塬区苹果园和农田相互转换的深层土壤水环境效应

研究长武塬区苹果园和农田相互转换后0~1 000 cm土壤含水量特征，分析了苹果园土壤干燥化和苹果园转换为农田后土壤水分的恢复效应。结果表明：2、7、17、23、29 a苹果园200~1 000 cm的平均土壤含水量分别为22.8%、21.4%、16.8%、15.4%、14.9%。500~1 000 cm土层中，29 a苹果园平均土壤含水量（14.5%）高于23 a的果园（13.3%）；17~29 a的苹果园均表现为轻度干燥化；基于苹果园和农田转换后土壤水分变化情况估算，苹果园最大种植年限为21 a。苹果园转换为农田1、5、10 a后，农田200~1 000 cm土层土壤含水量分别为：15.3%、15.7%和16.2%，恢复到土壤稳定湿度以上的土层厚度分别为140 cm（1 a）、220 cm（5 a）和400 cm（10 a）。