红外相机技术在河北雾灵山国家级自然保护区中的应用

为了充实河北雾灵山自然保护区的野生动物资源本底资料,提高监测能力和监测水平,雾灵山保护区自2015年开始将红外相机技术应用到野生动植物的资源调查和管护中。目前应用红外相机技术发现兽类5目10科14种,鸟类4目6科10种,掌握了区内主要物种猪獾(Arctonyx collaris)、狍(Capreolus)和勺鸡(Pucrasia macrolopha)的日活动节律,补充了保护区的本底调查资料,为保护区进一步开展金钱豹(Panthera pardus)、斑羚(Naemorhedus goral)和鸟类多样性等科学研究奠定了基础,为保护区制定关于野生动物资源的相关管护政策提供了科学依据。     

红鳞蒲桃开花物候特性研究

对红鳞蒲桃种群的花期物候，单株、单个花序、单花的开花动态进行系统的观测研究，详细测量并记录花部构件，同时调查红鳞蒲桃种群的同花期植物。结果表明：红鳞蒲桃种群的花期物候为8月1日～9月15日（2008年），持续时间46d；单株花期从23d到33d不等；单花序的花期情况较为复杂，总体表现为花朵数越多，该花序持续时间越长，但也有个别情况出现，在开花中期花序持续时间长，开花后期花序持续时间最短，开花前期花序持续时间介于两者之间；在整个种群花期内单花平均开花时间约5．2d，种群开花前期单花的持续时间约为6．7d，开花中期约为4．7d，末花期约为4．3d，种群开花前期单花的持续时间显著大于种群中后期的持续时间。红鳞蒲桃种群的同花期植物隶属于16科21属22种。     

The use of urban organic wastes in the control of erosion in a semiarid Mediterranean soil

Abstract. A two year field experiment was carried out in a semiarid Mediterranean area in order to evaluate, the effect on soil erosion of adding different urban organic wastes: a stabilized municipal waste (compost), an unstabilized municipal waste, and an aerobic sewage sludge. All the treatments significantly reduced soil erosion, compared to the control soil. The soil amended with compost was the most effective treatment, reducing soil loss by 94% and runoff by 54%.     

An evaluation of the pesera soil erosion model and its application to a case study in Zakynthos, Greece

Abstract. The Pan‐European Soil Erosion Risk Assessment (pesera ) model was evaluated using existing soil erosion data collected under various types of climate, vegetation, landscape and soil conditions. The data used represent a variety of typical Mediterranean land uses such as winter wheat, vines, olives and bare, stony land prevailing in hilly areas. Using this data, the model was calibrated for sediment transport by overland flow and results compared to measured soil erosion values from runoff plots and a watershed on a monthly basis. The performance of the model was assessed statistically, showing that it can be satisfactorily used for predicting soil erosion rates under the conditions included in the study. The overall model estimate including all the available experimental data was 0.69 t ha^?1 yr^?1 with a maximum error of 1.49 t ha^?1 yr^?1. After validation, the model was applied to a small watershed (60 ha) of great ecological importance for the sea turtle Caretta caretta. For this purpose, soil and vegetation maps were compiled from all the necessary data for applying the model. The model was run for three years using daily data from an existing nearby meteorological station. The predicted and measured soil erosion rates for a 7‐month period were 0.31 t and 0.18 t, respectively. Application of the model to each mapping unit showed the over‐riding importance of land use for sediment generation under the given climatic conditions. Bare land, occupying 5.5% of the watershed area, generated up to 69% of the total sediments estimated for the watershed. It is concluded that the pesera model can be used as a regional diagnostic tool under a range of soil, topographic and climatic conditions for identifying the best land use type and vegetation cover to protect hilly areas from soil erosion. The calculated overall root mean square error for the model is 0.06 t ha^?1 yr^?1, compared to a soil erosion rate of 0.04 t ha^?1 yr^?1, which can be tolerated for protecting the area for the sea turtle.     

Re-defining tillage erosion: quantifying intensity–direction relationships for complex terrain

Abstract. Current tillage erosion models account for the influence of tillage direction in the magnitude of the soil (tillage) transport coefficient. It is argued here that this is counter-intuitive and causes significant problems in modelling tillage erosion in areas of complex terrain. This article examines whether a re-modelling of tillage erosion is possible that separates tillage direction (an interaction with the landform) from the soil transport coefficient (a measure of tillage intensity representing the combination of implement erosivity and soil erodibility). Experimental data for mouldboard ploughing upslope, downslope and cross-slope at Coombe Barton Farm, Devon are examined. Integration of data for all directions into a single relationship, which relates translocation in the direction of tillage to slope in the direction of tillage and translocation perpendicular to tillage to slope perpendicular to tillage, is not possible using previously published methods of analysis. However, when total translocation distance is regressed against the tangent of the slope at 45° to the tillage direction (bisecting the tillage direction and the direction of overturning) it is found that a single relationship can be used to describe tillage in all three directions. Therefore, this relationship is used to determine a single value of the soil transport coefficient ( k _fTa) for constant soil and implement conditions but different tillage directions. This redefinition of tillage is important both for true estimation of tillage erosion severity, the adirectional coefficient being 40% larger than the directional coefficient, and for modelling of tillage erosion in complex terrain. These improvements are vital when tillage erosion simulation is used to direct soil conservation strategies.     

全国甘蔗野生种质资源的采集和考察

１９８５～１９９３年在全国进行了甘蔗野生种质资源的采集和考察。采集到甘蔗亚族（Ｓａｃｃｈａｒｉｎａｅ）内９个属１８个种的无性系共８２４份，种植在云南农业大学校园内（昆明黑龙潭），建立了甘蔗资源圃。考察了甘蔗属（Ｓａｃｃｈａｒｕｍ）、蔗茅属（Ｅｒｉａｎｔｈｕｓ）、河八王属（Ｎａｒｅｎｇａ）和芒属（Ｍｉｓｃａｎｔｈｕｓ）中主要野生种的地理分布、开花期、形态特征、繁殖方式、生态适应性、锤度和种质流失的情况。探明了割手密（Ｓ．ｓｐｏｎｔａｎｅｕｍＬ．）和斑茅（Ｓ．ａｒｕｎｄｉｎａｃｅｕｍＲｅｔｚ）的开花期与原产地纬度和海拔的相关，探索了割手密与蔗茅（Ｅ．ｆｕｌｖｕｓＮｅｅｓ）茎秆锤度与地理分布的联系。     

森林资源二类续档误差及原因分析

针对当前森林资源数据二类续档存在的问题,在对永安市大坑采育场大坑工区进行小班实地调查的基础上,以2003年初二类调查小班主要调查因子数据与1996年二类调查续档至2002年底数据进行对比,分析其误差及产生原因,并提出相关建议。     

土壤风蚀研究进展与评述

按照时间顺序，分阶段论述了国内外风蚀研究的概况及成果，系统地总结与评述了国内外土壤风蚀研究的进展，指出把土壤风蚀研究与农田耕作制度的研究结合起来，将是以后研究的重要方向。     

中国风水侵蚀交错区分布特征分析

风水侵蚀交错带的研究 ,对景观、土地覆盖 /土地利用、全球变化等研究具有重要意义。论文以GIS技术为支撑 ,定量计算出我国风水侵蚀带。在分布特征上 ,主要分布我国北方地区 ,其中以西部沙漠 ,北部山脉沿线为重 ,这种分布与气候、地貌分界有明显联系。 49.6 %风水侵蚀复合带的降水量小于 2 0 0mm。风水侵蚀复合带的土地利用主要以草地为主 ,占 41.8% ,其次为耕地。两种类型的分布 ,草地以与其它土地利用类型交错分布为主 ;而耕地是有重心的分散分布。风水侵蚀复合带的总体侵蚀要强于全国水平。     

西安白鹿塬约85OO年来土壤侵蚀研究

本文根据作者的观察和测量，对西安市白鹿塬塬区的土壤侵蚀状况进行了研究。研究表明，白鹿塬塬区确定土壤侵蚀的主要依据是土层厚度的变化，并非侵蚀面。塬区侵蚀是塬边侵蚀较强，向塬里侵蚀逐渐减弱。塬面上高地侵蚀弱，低地侵蚀强，暂时性线状流水长期汇集而成的冲沟对黄土塬区土壤的侵蚀更加强烈。气候对土壤侵蚀也有影响，冷干和温湿气候均会产生土壤侵蚀，冷干期侵蚀量比温湿期大，前者侵蚀厚度比后者大7倍多。