不同种植制度对稻田旱作季节CH4和N2O排放的影响

通过大田试验研究了稻田旱作季节几种典型种植制度对CH4和N2O排放的影响,包括休闲（fallow）、油菜对照（OR-ck）、小麦对照（W-ck）、油菜施N（OR-N）和小麦施N（W-N）5个处理。试验结果表明,稻田旱作季节N2O排放明显,CH4排放量较低,甚至表现为弱的CH4汇。稻田旱作季节N2O排放除受到N肥和种植制度影响外,还受土壤含水量影响,施N处理显著促进了N2O排放,降雨后N2O排放明显。小麦和油菜施N处理N2O平均排放通量分别为18.51和13.47μg·m^-2·h^-1,季节累积排放量分别为87.31和59.48 mg·m^-2,均显著高于对照和休闲处理。不同作物种类间N2O平均排放通量无显著差异,N2O季节累积排放量则表现为小麦显著高于油菜。各处理综合温室效应（100 a）依次为：OR-N〉W-N〉W-ck〉fallow〉OR-ck。各施N处理综合温室效应以N2O为主,但各无N处理则以CH4为主,也不容忽视。     

Modelling dynamics of soil organic matter under different historical land-use management techniques in European Russia

We have analyzed an influence of the traditional agricultural system techniques on the soil organic matter dynamics using the model of carbon and nitrogen cycling in forest ecosystems EFIMOD linked with the model of SOM dynamics ROMUL. Forest stands on the loamy soddy-podzolic soils (Alfisoils) located in the Central European Russia have been taken for the case study. The following land-use management scenarios were simulated: (a) slash-and-burn system with 3 years for crops and 120, 60 and 25 years for forest; (b) three-field crop rotation system with organic fertilization (dung) every 3 and 9 years and the same rotation without fertilization; and (c) short-term field-forest shifting system with 10 years for crops and 10 and 25 years for forest. Analysis of the results showed that the frequency of agricultural use in mixed field-forest land-use systems was crucial for soil organic matter dynamics. Under the short interval between agriculture, the stocks of all soil organic matter pools decreased. Under all scenarios except the three-field crop rotation with fertilization and the slash-and-burn system with 120 years for forest, a strong reduction of soil organic matter occurred after 30-130 years of the agricultural impacts. The highest reduction rates were modelled under the short-term field-forest shifting system and three-field rotation without fertilization. Fertilization led to stabilization of soil organic matter pools and gave a possibility for a long time stable agricultural use.     

Traditional crop diversity for sustainable development of Central Himalayan agroecosystems

SUMMARY

A rich diversity of traditional crops occurs generally in the Himalaya and more particularly in Central Himalaya. Over forty species of food grains are grown in traditional agroecosystems of Central Himalaya, which have been managed by the local farming communities since time immemorial. These traditional crop varieties have evolved over centuries and are well adapted to the particular area. A number of edaphic, topographic and climatic factors associated with different selection pressures over centuries of cultivation resulted in immense variations in the crop species.

The grain and by-product yield of the majority of the traditional crops cultivated across an altitudinal gradient were worked out and compared with common food crops (paddy, wheat, mustard) at two points in time (1970-74, 1990–94) and it was found that almost all the traditional crops had slightly higher yields during 1970–74 than between 1990–94. However, common food crops grown during the Kharif season had higher yields during 1990–94 whereas, Rabi season crops exhibited higher yield during 1970–74. The yield of rainfed paddy remained static over the years across the altitudinal gradient. Among the traditional crops cultivated during the Kharif and Rabi seasons in mixed and pure forms at different altitudes were Macrotyloma uniforum (at higher altitude), Parilla frutescens and Vigna mungo (at middle altitude) and Panicum miliaceum (at lower altitude) which were found to be eco-energetically efficient. Avena sativa (oat) and mixed cropping of Fagopyrum esculentum and potato had higher energy efficiency ratios whereas the latter also exhibited a higher monetary output/input ratio. Crops like paddy and wheat with mustard, grown in irrigated land were found to be more eco-energetically efficient than the same crops grown in the rainfed land. In general, traditional crops possess higher nutritive value than the common food crops. The contribution of traditional crops to the local diet (kg/capita/year) and their energy and protein equivalents were higher during both time periods. It was observed that while exporting these traditional crops, the locals of the region are highly exploited by middlemen. Despite having huge potential, traditional crop diversity of this region has been reduced to a great extent during the last two decades. Besides, the area under cultivation with these crops has been declining rapidly. However, many of these crops possess immense potential to meet the growing food demand and ensure food security of an increasing population. Therefore, a comprehensive programme of conservation through various means and improvement of agronomic yield in their natural habitats is urgently needed.     

大城市郊区典型区域农户作物种植选择行为及其影响因素对比研究——基于沈阳市苏家屯区238户农户的调查研究

研究从农户作物种植选择行为角度出发,以马斯洛需求层次理论为基础,通过构建社会经济及政策变化对农户种植选择行为影响机理分析框架和理论模型,基于沈阳市苏家屯区238户农户调查数据,采用统计分析法和Logistic回归分析,研究结果表明:工业化、城市化进程的加快促进了大城市郊区非农就业机会的增多和对农产品需求的增加,导致农户作物种植业选择行为出现了明显的"非粮化"和"非农化"趋势,不同区域农户作物选择行为存在明显的差异,在空间上形成近郊区以种植粮食作物为主→远郊区兼种粮食作物和经济作物为主→纯农村区以种植经济作物为主的"反杜能圈"式的种植模式特征。在此研究基础上,从外部环境包括城市扩展、经济结构、市场价格变化、政策制度安排和内部环境包括个人特征、家庭特征、资源禀赋等7类因素13个因子对产生差异的影响机理进行分析,结果显示不同区域、不同因子的作用方向、影响程度与显著性表现均有所不同。根据以上的研究结果,政府应该从鼓励农户发展休闲农业、合理引导农户把握市场和培养新型农民等方面入手,优化农业结构调整,促进农村土地合理利用,提高土地利用效率,实现农村土地资源的持续利用。     

内蒙古典型草原作物系数和实际蒸散量的时空分布特征

利用内蒙古典型草原21个气象站点的气象和牧草观测资料,结合潜在蒸散量和改进的作物系数计算方法,模拟计算了2009年草原植被作物系数和实际蒸散量.在GIS软件的支持下,分析了二者的时空分布特点,并通过反映牧草长势的NDVI变化趋势予以验证.结果表明:5-8月间随着月份的增加作物系数Kc_x最大值的变化趋势由0.6→1.2→1.4→1.4,平均值是0.28→0.36→0.40→0.38.4个时期的Kc_x值以0.2~0.6之间的区域占主体,为55%以上.实际蒸散量在时间变化和空间分布上与Kc_x值基本一致.随着月份的增加实际蒸散量低值级的区域面积逐渐缩小,相对应的高值级的面积逐渐增大,整个生长季以30~90 mm的蒸散量为主.5-8月牧草实际蒸散量和NDVI值的相关系数达到0.446,通过了0.01水平的显著性检验.     

施氮水平对小麦-玉米轮作体系氨挥发与氧化亚氮排放的影响

试验采用密闭室间歇通气法研究华北平原冬小麦（Triticum aestivum Linneaus）-夏玉米（Zea mays Linneaus）轮作体系在不同施氮水平下农田氨挥发和N2O排放。结果表明：冬小麦季和夏玉米季的氨挥发速率与N2O排放通量呈现出季节性动态变化,且随着施氮量的增加而增加,均在施肥后第2~3天出现峰值。玉米季氨挥发量和N2O排放量均高于小麦季,分别占整个轮作周期气态损失的53.5%~68.9%和54.7%~82.3%。轮作体系中氨挥发净损失量（以N计）为4.28~31.31 kg.hm-2,占施氮量的3.17%~5.80%;N2O净排放损失量（以N计）为50.95~1051.03 g.hm-2,占施氮量的比例为0.04%~0.23%。因此,施氮量是影响冬小麦-夏玉米轮作体系气态损失重要因素,且夏玉米季是控制控制气态损失的关键时期。     

不同作物原料热裂解生物质炭对溶液中Cd2＋和Pb2＋的吸附特性

选择由小麦秸秆、玉米秸秆和花生壳经350-500℃热裂解制成的生物质炭,研究生物黑炭对水溶液中Cd2＋和Pb2＋的吸附特性,分析了pH值、吸附时间、溶液初始质量浓度、生物质炭粒径和投加量对吸附效果的影响。结果表明：生物质炭对Cd2＋和Pb2＋的吸附约10 min即达平衡;3种生物质炭对Cd2＋和Pb2＋的等温吸附均可用Langmuir方程和Freundlich方程拟合,玉米秸秆炭对Cd2＋和Pb2＋的最大吸附量远大于小麦秸秆炭和花生壳炭;在生物黑炭投加量为150 mg（6 g.L-1）时,3种生物黑炭对溶液Cd2＋的去除率均在90%以上,玉米秸秆炭对溶液Pb2＋的去除率达90.30%,而小麦秸秆炭和花生壳炭的去除率仅为52%和47%,玉米秸秆炭有望成为处理重金属污染废水的新型吸附材料。     

矿粮复合区土壤-作物系统重金属污染风险性评价

为分析矿区污染农田农作物生产的生态安全性,以焦作市中马村矿区的典型农田为例,对矿区农田土壤及植物中Zn、Cr、Cd、Cu和Pb等重金属的质量分数进行了测定,并对重金属污染风险进行了评价。结果表明,根据重金属的单项污染指数,在矿井水污灌农田（F1样地）土壤中Zn和Cd的质量分数达到中度污染水平,Cr的质量分数达到轻微污染水平,Cu和Pb元素质量分数未达到污染水平。在煤矸石污染农田（F2样地）土壤中Zn、Cr和Cd的质量分数达到轻度污染水平,Cu和Pb元素质量分数未达到污染水平。在矿区公路侧农田（F3样地）土壤中各元素质量分数均未达到污染水平。采用潜在生态风险指数法对土壤重金属污染的生态风险进行评价,F1和F2样地综合生态风险指数分别为239．60和178．42,达到中等水平,F3样地土壤达到轻微生态风险水平。采用单项污染指数和综合污染指数法对小麦（Triticumaestivum）籽粒中重金属风险进行评价,在F1和F2样地中,小麦籽粒中Cu质量分数均未达到污染水平,Pb、Cd和Cr质量分数均达到重度污染水平。Zn质量分数在Fl样地中达到轻度污染水平,在F2样地中达到中度污染水平。在F3样地中,小麦籽粒中Cd和Cu质量分数未达到污染水平,Zn质量分数达到轻度污染水平,Pb、Cr质量分数达到重度污染水平。从综合污染指数评价来看,F1、F2和F33个样地小麦籽粒中重金属污染综合指数均达到重度污染水平。评价结果对科学治理矿区污染土壤,确保矿区农田生态安全、粮食生产安全具有重要意义。     

连续周年轮作休耕对土壤团聚体稳定性及有机碳的影响

为探究连续周年轮作休耕对红壤团聚体稳定性及有机碳含量的影响,以坡耕地红壤为研究对象,采用湿筛法和重铬酸钾-浓硫酸外加热法分别测定水稳性团聚体和有机碳含量,分析了2020~2022年玉米-苕子-玉米轮作（M-V-M）、玉米-豌豆-玉米轮作（M-P-M）、玉米-冬闲-玉米（M-F-M）和周年休耕（F-F-F）这4个处理下土壤团聚体稳定性及有机碳含量变化特征以及两者间的相互关系.结果表明,在2021年和2022年中,F-F-F、M-V-M和M-P-M处理的> 2 mm团聚体含量较M-F-M分别显著提高了67.01%~100.92%、29.71%~33.67%和29.68%~38.07%;2021年和2022年中F-F-F、M-V-M的团聚体稳定性参数显著高于M-F-M（P < 0.05）.M-V-M处理下的> 2 mm团聚体含量、GMD（几何平均直径）和MWD（平均重量直径）及F-F-F处理的R_0.25（ > 0.25 mm团聚体含量）、MWD和> 2 mm团聚体含量随着轮作休耕年限的延长而增加,而F-F-F处理下1~2 mm和< 0.25 mm团聚体含量随着休耕年限的增加而降低.绿肥轮作和休耕处理均能够提高SOC含量,且F-F-F和M-V-M处理的SOC含量随年限的延长而增加.相关性分析表明,所有处理下SOC含量与R_0.25呈极显著正相关,与GMD呈显著正相关;F-F-F处理下的R_0.25和GMD及M-V-M处理下的GMD和MWD均与SOC含量显著正相关.结果表明,连续周年轮作休耕有利于提高土壤大团聚体含量、团聚体稳定性和SOC含量,可为我国南方坡耕地红壤区推行合理的连续周年轮作休耕模式和水土流失防治提供理论依据.     

Accumulation of heavy metals in soil and paddy crop (Oryza sativa), irrigated with water of Ramgarh Lake,Gorakhpur, UP,India

Heavy metals, a highly polluting group of constituents known to exert adverse effects, tend to accumulate in living organisms. The objective of this study was to determine the accumulation and translocation of heavy metals in soil and in paddy crop irrigated with lake water compared to soil and paddy crop irrigated with bore-well water. The quantities of heavy metals (Cd, Cr, Cu, Pb, Zn, As, Mn, and Hg) were determined in different parts of rice plants (Oryza sativa). Results revealed that the mean levels of soil Cd, Cr, Pb, Zn, As, Mn, and Hg in experimental soil and in different parts of rice plant (root, straw, and grain) were higher than the control except for Cu. The content of eight toxic metals was significantly higher in root than in aerial parts of the rice (straw and grains). Rice roots were enriched in Cd, As, Hg, and Pb from the soil, while Cr, Cu, Zn, and Mn were hardly taken by the roots. Bioaccumulation factor for Hg was significantly higher than other heavy metals. Metal transfer factors from soil to rice plants were significant for Cd, Cr, Cu, Pb, Zn, As, Mn, and Hg. The concentrations of metals in lake water were found to be within the permissible limit of Indian standard prescribed by Central Pollution Control Board (2000), except for Hg and As, which were higher than the limit of Indian standard. However, the concentrations of heavy metals in soil and rice grains were still below the maximal levels, as stipulated by Indian Prevention of Food Adulteration Act (PFA, 1954) and World Health Organization (WHO, 1993) guidelines.