我国不同奶业产区规模化牧场饲料结构分析

在奶牛养殖规模化水平不断提高,养殖成本日益增加,且区域间差异明显的背景下,饲料作为奶牛养殖主要投入品,了解其在规模化牧场生产成本中的结构对于优化奶牛日粮结构、降低养殖成本、缩小区域间养殖效益差距等具有重要意义。本文利用2018—2020年规模牧场月度调研数据,分析了我国规模化牧场饲料结构情况。研究发现,大城市周边产区和南方产区的精饲料和粗饲料的比例相对更加科学,华北产区仍有较大提升空间,并且玉米、豆粕、玉米青贮和苜蓿草在日粮中占有较大比重,达到84.62%;不同产区奶牛日粮结构具有明显差距,玉米青贮和苜蓿草在西北产区占比最高,玉米和豆粕在南方产区占比最高。注重发挥区域优势,加大优质粗饲料和可替代饲料的利用,有利于降低养殖成本,提高养殖的科学性和可持续性。     

The River Wadu role play — ten years experience

This paper describes a role playing planning exercise that has been used for training agriculturists, engineers and agricultural economists for more than ten years. It sets out the objectives and key features of the exercise and the experience that has been gained in its use. The exercise has been found to successfully test and integrate subject matter expertise acquired from formal teaching. It also highlights the multiple and often conflicting objectives of irrigation planning, and the need for full evaluation of alternatives and sound technical judgements under conditions of inadequate data and time pressure. The exercise is also successful in developing professional personal skills such as group working, interviewing and presentation, and is recommended as an effective training aid.     

旱田中耕节水灌溉设备的研究

分析了节水灌溉现状；以玉米苗期为研究对象，结合黑龙江省旱作农业实际，提出了一种与中耕相结合的灌溉方式，为采用机械化灌溉方法解决作物苗期干旱问题提供参考。     

Changing technology for training irrigation managers

This article describes developments in microcomputer and video-disc technology which may be used in the training of managers for irrigation projects.     

棉花冠层叶面积的动态模拟

根据试验资料,在系统分析棉花冠层叶面积时空分布规律的基础上,充分考虑叶面积空间垂直分布的异质性,以生育期内累积的每日相对热效应为预报因子,构建了棉花叶面积垂直分布和叶面积指数的动态模拟模型。利用不同年份不同播期的试验资料对模型进行了验证,累积叶面积指数L（z）的模拟结果与1∶1直线之间的R^2和均方根误差分别为0.969和0.257,叶面积指数LAI的模拟结果与1∶1直线之间的R^2和均方根误差分别为0.936和0.305。结果说明模型具有较好的预测性和实用性。模型的模拟结果可作为冠层结构参数,用于冠层辐射传输模型和光合作用模型。     

桃林口水库供水效益分析计算

主要分析了桃林口水库的农业灌溉、工业城市供水的国民经济效益，分别计算出水库单方农业灌溉供水和工业城市供水国民经济效益值。在水利工程经济效益分析方法、理论有新的探索，对类似工程效益分析有一定的借鉴意义。     

平地漫灌灌溉水净化与循环利用研究

为提高设施农业的水分利用率，设计了平地漫灌灌溉水净化与循环利用系统；阐述了系统的组成、节水灌溉原理与工作过程。理论分析可知，系统具有较高的输水利用率、灌水利用率和降水利用率，是农业节水灌溉的有效新途径。     

CO2加富及亏缺灌溉对菜豆中期与后期生长的影响

为了探明菜豆中期与后期生长对CO₂加富与亏缺灌溉的生理响应,试验设两个CO₂水平:正常大气浓度和倍增CO₂浓度,两个灌溉水平:自然灌溉12次和亏缺灌溉6次,研究CO₂加富及亏缺灌溉对菜豆生长的影响。结果表明,CO₂加富显著提高菜豆生长中期株高与干质量,净光合速率(Pn)与胞间CO₂浓度(Ci)分别显著降低15.48%、37.67%,气孔导度(Gs)显著提高95.83%,菜豆生长后期的叶绿素a/b(Chla/b)显著提高12.29%,水分利用效率(WUE)显著提高46.51%,Ci显著降低12.87%。CO₂加富显著提高亏缺灌溉下生长中期菜豆的株高与干质量,但显著降低根冠比,显著提高叶绿素含量以及Gs;CO₂加富下生长后期的核酮糖-1,5-二磷酸羧化酶(Rubisco)及果糖-1,6-二磷酸酶(FBPase)活性分别显著提高78.05%与88.69%,CO₂加富使亏缺灌溉下碳酸酐酶(CA)与FBPase活性分别显著提高83.73%与64.84%。综上所述,CO₂加富提高菜豆生长中期对亏缺灌溉的适应性,对生长后期影响作用减小。     

Change features of time-series climate variables from 1962 to 2016 in Inner Mongolia,China

Detecting change features of climate variables in arid/semi-arid areas is essential for understanding related climate change patterns and the driving and evolution mechanism between climate and arid/semi-arid ecosystems.This paper takes Inner Mongolia of China,a unique arid/semi-arid ecosystem,as the study area.We first detected trend features of climate variables using the linear trend analysis method and then detected their trend-shift features using the breaks for additive seasonal and trend method based on the time-series of monthly precipitation and monthly mean temperature datasets from 1962 to 2016.We analyzed the different change features of precipitation and temperature on a regional scale and in different ecological zones to discover the spatial heterogeneity of change features.The results showed that Inner Mongolia has become warmer-wetter during the past 54 years.The regional annual mean temperature increased 0.4°C per decade with a change rate of 56.2%.The regional annual precipitation increased 0.07 mm per decade with a slightly change rate of about 1.7%,but the trend was not statistically significant.The warmer trend was contributed by the same positive trend in each season,while the wetter trend was contributed by the negative trend of the summer precipitation and the positive trend of the other three seasons.The regional monthly precipitation series had a trend-shift pattern with a structural breakpoint in the year 1999,while the regional monthly mean temperature series showed an increasing trend without a periodical trend-shift.After the year 2000,the warmer-wetter trend of the climate in Inner Mongolia was accelerated.The late 20th century was a key period,because the acceleration of the wetter trend in some local zones(I and II)and the alleviation of the warmer trend in some local zones(Ⅶ,Ⅷand IX)occurred simultaneously.Moreover,the change features had a strong spatial heterogeneity,the southeastern and southwestern of Inner Mongolia went through a warmer-drier trend compared with the other areas.The spatio-temporal heterogeneity of the climate change features is a necessary background for various types of research,such as regional climate change,the evolution of arid/semi-arid ecosystems,and the interaction mechanisms between climate and arid/semi-arid ecosystems based on earth-system models in Inner Mongolia.