基于HACCP的粮食质量安全网络监测平台研究

保证粮食质量安全对我国食品安全具有举足轻重的意义,为实现全程质量监控,确保粮食在各个环节的质量安全,需加强对粮食质量安全领域的监管力度,建立粮食质量安全保障体系,构建一个基于HACCP的粮食质量安全网络监测平台,实现粮食质量安全各个环节的透明化和信息化。     

保护性耕作对小麦-土壤系统综合效应研究

采用长期定位试验与短期田间试验相结合的方法,通过室内化验分析和数理统计,研究了河南省不同土壤类型区保护性耕作对土壤理化性质、土壤微生物生物量碳氮及小麦(Triticum aestivum L.)籽粒产量和产量构成因素的影响。结果表明,与传统耕作相比,保护性耕作显著提高土壤有机质、碱解氮、有效磷及交换性钾含量,分别提高24.8%、14.3%、7.8%和24.8%;而对小麦增产效果并不显著。4种不同保护性耕作方式下,免耕、浅耕相比旋耕、深耕,提高小麦穗数15.0%～32.2%,提高穗粒数2.6%～12.6%,但4种处理间小麦千粒重及籽粒产量效果无显著差异;免耕、浅耕较旋耕、深耕可以一定程度上提高苗期和灌浆期土壤含水率、以及土壤碱解氮和有效磷,并显著提高小麦不同生育时期的土壤微生物生物量碳氮。免耕与浅耕是较为适宜河南省小麦生产及土壤可持续利用的保护性耕作方式。     

基于人粮关系的湖南省耕地资源人口承载力研究

从人粮关系角度估算土地生产潜力,对耕地资源人口承载力进行研究,对保障国家粮食安全和区域可持续发展都具有十分重要的意义。通过应用土地资源人口承载力和土地资源人口承载指数模型研究了湖南省2000—2008年耕地资源的人粮关系状况,结果如下:(1)在现有生产力水平下,湖南省耕地资源可承载人口7 423.38万人,人口承载力指数为0.922,人粮关系基本平衡,但人粮关系状况分布不均衡,地区差异较大。(2)湖南省中北部、西部和南部3大区域耕地资源人口承载力2000—2004年处于逐年下降趋势,之后则逐年上升。(3)中北部人粮关系2004年后由盈余状态转为富裕状态,西部一直处于超载和临界超载的边缘,南部则多为盈余状态。表明湖南省耕地资源人口承载力地区差异较大,人口增长空间十分有限,今后应加强土地综合整治,改善土地生产条件,提高农业科技水平,以实现区域资源、人口与环境的可持续发展。     

Effect of phosphorus fertilizer application on the performance of maize/soybean intercrop in the southern Guinea savanna of Nigeria

Field experiments were conducted at the Teaching and Research Farm, Ladoke Akintola University of Technology, Ogbomoso, Nigeria in 2007 and 2008 to determine the effects of phosphorus fertilizer application on performance of intercropped maize and soybean. The experiments, arranged as a split plot in a randomized complete block design, replicated four times. A cropping system with sole maize, sole soybean and maize/soybean intercrop formed the main plot treatments while P rates with 0, 15 and 30 kg P₂O₅ ha^?1 were the subplot treatments. For both years, neither P fertilizer application nor cropping systems had a significant effect on maize grain yield. However, soybean grain yield was significantly higher (92.3% in 2007 and 44.5% in 2008) under sole cropping than under maize/soybean intercropping. On average, N fixed by soybean increased with the increase in P rate (from 51.8% without P to 60.5% with 30 P), but there was no significant difference in N fixed by sole soybean and soybean/maize intercrop. However, the interaction effect on N fixed between cropping systems and P rates was significant (P ≤ 0.05). N, P and K contents in maize grain were significantly higher (>100%) in intercropped maize than in sole maize. The cropping systems had no significant effect on post-harvest soil chemical characteristics. The land equivalent ratio was 1.52 in 2007 and 1.78 in 2008. The result shows that in utilizing legumes for N enrichment, the alleviation of P deficiency can enhance N₂-fixation by legumes. Furthermore, P replenishment in a maize/soybean intercrop may improve maize grain quality even though yield is not increased.     

基于机器视觉的玉米果穗参数的图像测量方法

在玉米育种和品质研究中,经常需要对玉米的果穗长度、果穗宽度、穗行数、穗粒数等参数进行测量。该研究提出了一种基于机器视觉的玉米果穗参数图像测量方法。使用PC摄像头连续采集旋转台上的玉米果穗图像,经过图像处理,获得玉米穗的图像区域,进而得到玉米果穗的穗长和穗宽参数;通过对玉米果穗局部区域的x方向和y方向累计像素值曲线进行分析,提取出玉米穗行,获得每一穗行的穗粒数和穗行宽度;通过图像匹配,获得玉米果穗的穗行数。试验表明,使用该研究方法对玉米果穗的长度、宽度和穗行数的参数测量准确率可达98%以上,对穗行宽及总穗粒数测量准确率达95%以上,整穗的平均检测时间约102 s/穗。该研究实现了玉米果穗参数快速有效的自动检测,相对于目前采用的人工检测,大大提供检测效率,降低劳动强度,可应用于玉米千粒质量检测、产量预测、育种和品质分析等场合。     

黄土高原丘陵区退耕还林地土壤碳氮库的动态变化(英文)

为了揭示坡耕地退化土壤植被恢复后土壤中碳(C)、氮(N)运移规律,采用植被次生演替空间序列代替时间序列的方法,研究了黄土丘陵沟壑区纸坊沟流域不同植被恢复模式下的C、N库及其相互关系在土壤剖面的时空变化。结果表明退化农地的造林显著地促进了CO2的固存,恢复了土壤N的可获得性,进而降低了N不足对可持续的CO2固存的限制。植被恢复显著地促进了0~60 cm土壤有机碳(soil organic carbon,SOC)和总氮(total nitrogen,TN)的积累,而只有在高于一定的恢复时间阈值(如26 a)下,促进了SOC库和TN库间的线性相关性。在土壤剖面上,SOC和TN库、SOC/TN库比以及SOC-TN间的线性相关性均随着土壤深度的增加而降低。与自然恢复相比,人工林在短期内具有CO2固存的优势,但由于随着恢复时间的增加,SOC增幅越来越大于TN增幅的事实,表明造林对碳固存的可持续性需在一个较长的时段下来评估,尤其需要关注20 cm以下层土壤。研究结果为黄土高原的生态修复和减缓温室效应提供了理论依据。     

灌水量和时期对不同品种冬小麦产量和耗水特性的影响

为明确品种更替过程中冬小麦的耗水特性、产量和水分利用效率(WUE)的变化规律,以及对水分胁迫的响应,于2010-2012两个生长季选取河南中北部建国以来不同年代的7个主栽品种为试验材料,在田间设置三个水分处理下(W0,返青后不灌水;W1,拔节期灌水;W2,拔节和灌浆期分别灌水),研究了冬小麦的耗水特性、产量构成因素、收获指数和水分利用效率的变化过程。研究结果表明:在冬小麦更替过程中,冬小麦总耗水和土壤贮水消耗与年代差异不显著,而受降雨和灌溉影响较大。从20世纪50年代至现在,90年代及以后的冬小麦品种千粒重在41g以上,明显高于早期品种。两年生长季冬小麦籽粒产量增加58.4%和41.8%,平均每次更替增加396和362kg/hm2;收获指数增加37.0%和18.0%,平均每次更替增加0.2和0.1;WUE增加55.3%和40.8%,平均每次更替增加0.11和0.10kg/m3。现代品种源、库关系得到改善,千粒重大幅度增加和收获指数增加是籽粒产量提高的主要原因。籽粒产量和WUE由品种和水分互作效应决定,在拔节期和灌浆期灌水可明显提高籽粒产量水平,并在一定程度上提高了水分利用效率。     

延安地区降雨引发黄土泥流的试验研究

在野外模拟降雨条件下,研究了黄土粒度分布和微结构在降雨前后的变化及其对泥流启动的影响.结果表明,采自径流沉积物的降雨后土样中的细黏粒、粗黏粒体积含量分别相对增加了22％和18％,而粗粉粒、微砂体积含量分别相对减少了7.6％和3.3％.坡面残余土的粒度“粗化”,降雨后土骨架连接松散,这些由降雨引起的黄土的粒度和微结构变化说明降雨后黄土的抗剪强度和抗压能力将降低,导致泥流启动的可能性增加.随着降雨入渗,当沿坡面的黄土重力分力与抗剪强度间的平衡被打破,黄土开始滑移并发展成泥流.有效防止坡面土粒度“粗化”是遏制水土流失的关键.     

Prediction of grain protein content in winter wheat through leaf color measurements using a chlorophyll meter

A field trial was conducted over a 3-year period at the Hokkaido Kitami Agricultural Experiment Station to examine whether the grain protein content (GPC) of a winter wheat cultivar (Triticum aestivum L. cv. Chihokukomugi) suitable for Japanese noodle-making could be predicted before harvest. The prediction of the GPC was accurate based on the color of the second leaf (just below the flag leaf) at the end of the emergence of the inflorescence, when nitrogen application was graded. In order to evaluate the reliability of this test, a survey of 95 wheat fields in the eastern part of Hokkaido was also carried out during a 3-year period. The prediction of the GPC for this cultivar based on the color of the second leaf was less accurate across many sites. The results of this survey, however, suggested that the leaf color could be used as an index for ranking the GPC as low or high in relation to processing requirements. When the leaf color value of the second leaf measured with a chlorophyll meter at the end of the emergence of the inflorescence was less than 40, it was predicted that the GPC would be lower than the processing requirement. This index could be applied to the cultivars grown in the eastern part of Hokkaido, except for those grown on peat soils.     

Asymmetric warming effects on N dynamics and productivity in rice (Oryza sativa L.)

Climate warming exhibits strong diurnal variations, with higher warming rates being observed at nighttime, which significantly affects rice (Oryza sativa L.) growth and grain yield. The objective of this study was to determine the effects of asymmetric warming (all-day warming, AW; daytime warming from 07:00 to 19:00, DW; nighttime warming from 19:00 to 07:00, NW, and a control, CK) on rice nitrogen (N) dynamics and productivity. Two rice bucket warming experiments were performed in Nanjing in Jiangsu Province, China, using the free air temperature increase (FATI) technique. The daily mean temperatures in the rice canopy in the AW, DW and NW plots were 2.0, 1.1 and 1.3ºC higher than those in the rice canopy in the CK plots, respectively. The results indicated that the total N accumulation of rice was 8.27–40.53% higher in the warming treatment than in the control during the jointing, anthesis and maturity stages. However, there was no significant difference detected among the three warming treatments. The warming treatment substantially decreased N translocation efficiency, leading to the retention of more N in the plant stems during grain filling. The warming treatment also decreased the N harvest index, N utilization efficiency based on grain yield and N utilization efficiencies based on biomass in both growing seasons. The warming treatment significantly increased the aboveground biomass (9.26–16.18%) in the jointing stage but decreased it (2.75–9.63%) in the maturity stage. Although DW increased the carbon (C) gain by photosynthesis and NW increased the C loss by night respiration, the daytime higher-temperature treatment affected rice photosynthesis and reduced its photosynthetic rate and product. This effect may be one of the primary reasons for the insignificant difference in the aboveground biomass between the DW and NW treatments. In the AW, DW and NW plots, the grain yield was reduced by an average of 10.07, 5.05 and 7.89%, respectively, across both years. The effective panicles and grains per spike tended to decrease in the warmed plots, whereas irregular changes in the 1000-grain weight were observed. Our results suggest that under the anticipated climate warming, rice productivity would further decline in the Yangtze River Basin.