双孢蘑菇覆土层有益微生物消长规律

将土样制备成稀释液，采用平板涂布培养法，分析双孢蘑菇覆土期、充分发菌期，原基形成期、采收前和采收后2d5个时期土样中几种有益微生物和消长规律。结果表明，原基表成前和采收后，采白色和采收后2d5下时期土样中几种有益微生物的消化规律。结果表明，原其开前和采收后，采白色孢杆菌(Bacillus)、固氮苗（Azotobacter)和假单胞杆菌（Pseudomonas)数量增加；链霉菌（Streptomyces)数量增减比较平缓，而土灰色芽孢杆菌的数量一直呈下降趋势。     

Effects of 'Agri-SC' soil conditioner on soil structure and erodibility: some further observations

Abstract. In field and laboratory experiments the conditioner‘Agri-SC’has shown improvements in the structure of loamy sand soils in east Shropshire, UK. It resulted in statistically significant decreases in soil bulk density values and increases in soil porosity and aggregate stability. Further experiments are in progress on both loamy sand and silt loam soils.     

菲律宾以稻为基础的种植制度生态学评价 Ⅰ.各类种植方式的养分平衡

在菲律宾的雨养旱地、雨养低地和灌溉田种植制度研究基点上,分别对各种农民和拟推广的实验种植方式,进行了生物量及其组成、作物分器官的 C、N、P、K 含量与分布比率、作物残茬燃烧后 C、N、P、K 损失测定。从添加与取走两个方面,分三种添加与取走情况,计算了土壤N、P、K 的部分养分平衡与有机质平衡。结果显示:在当地施肥水平下,即使归还全部残茬,很难维持 N、P、K 的养分平衡,但能较好满足土壤有机质平衡。为维持土壤有机质的年平衡,雨养低地和雨养旱地需分别归还1400和1900公斤生物物质/公顷.年。并对当地维持养分平衡的途径作了分析与探讨。     

大豆室内耐冷筛选及其在田间的应用研究

本试验把生长箱大豆耐低温萌发筛选与田间早春播研究相结合,验证耐低温发芽的可靠性。在实验室,萌发期表现抗冷的大豆,田间出昔期仍表现抗冷或较抗冷。实验表明,大豆出苗的生物学最低温度平均为7.1℃,所需有效积温136℃。地温的高低直接影响大豆早春出苗的多寡,两者呈密切的正相关。黄、青、黑豆中,以黑豆抵抗早春不良气候条件的能力最强。     

北京中山地区非石灰性土壤发生分类的研究

利用剖面形态、微形态、理化分析、粘粘x衍射分析等结果,对北京中山地区土壤的发生过程和分类问题进行了研究。首次提出尘暴降尘物质对土壤发生过程的滞缓作用。若土壤分类上采用pH(KCI),北京中山地区非石灰性土壤应属于暗棕壤。在土壤分类特征上,为在山地普遍应用中避免估算和推测造成混乱,建议采用反映该地区水分和温度状况的植被。     

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.     

沙土区薄壁连拱护岸墙试验与应用

沙土区薄壁连拱护岸墙为悬臂式支撑、薄壁连拱无底板结构，拱板中间采用无砂砼排水孔的钢筋砼肋形预制板，冲沉法施工，造价低廉；外形美观，抗倾、抗滑性能强。该墙为平原沙土区河道水土保持及修复找到了一条经济合理、施工方便、简便易行的护坡办法，具有较高的实用价值和广阔的推广使用前景。     

台江采育场竹木混交林丰产措施试验

对台江林业采育场现有竹木混交林进行施肥和土壤垦复两种试验，结果表明，不同施肥处理虽有一定增产效果，但经方差分析未达到显著水平；不同土壤垦复措施的增产效果，以深翻加施肥的新竹产量最高，锄草松土居第二，单纯深翻并不理想，效果不如劈山抚育。因而，新兴竹木混交林应以调整竹林结构和护笋养竹为主，每年锄草松土即可达到材用丰产林标准，不宜盲目深翻、施肥。     

四川省退耕还林模式初探

根据自然地理分异规律、社会经济技术原理、生态学原理,分析了四川省的水土流失概况,提出了川中丘陵、盆周山地区、川西南干热干旱河谷区、川西北高山高原区的退耕还林模式。     

不同的施肥方式对剑麻施肥区域土壤微生物类群的影响

研究不同的施肥方式对剑麻施肥区域土壤微生物类群产生的影响。结果表明，不同施肥方式下土壤微生物总量各有差异，在总体数量上以细菌为主，真菌次之，再其次是放线茵，特殊生理类群是解磷茵居多，纤维素分解茵次之，固氮茵最少；但从土壤微生物多样性指数来看，则表现为土壤中主要微生物类群多样性指数是施肥点的土壤高于附近的土壤，而土壤中特殊生理微生物多样性指数则无此变化趋势，即微生物总数高的土壤，其多样性指数不一定高。因此评价土壤生物多样性应将二者结合起来。