水稻与稻瘟病菌非亲和性互作中重要防御酶活性变化规律研究

 选以CO39为背景的水稻抗稻瘟病近等基因系,与稻瘟菌生理小种ZC₁₃(菌株97-151a)组成的3类典型非亲和性互作,以亲和性互作为对照,对各互作中过氧化物酶(POD)、苯丙氨酸解氨酶(PAL)、几丁质酶及β-1,3-葡聚糖酶的活性变化规律进行了系统研究。完全非亲和性互作C101A51/97-151a、高度非亲和性互作C101L AC/97-151a及中度非亲和性互作C104 PKT/97-151a,POD比活性接种后即开始明显升高,48h前达到高峰,升高趋势一直持续到7d完全显症时,幅度基本与各互作非亲和程度呈正相关;亲和性互作CO39/97-151a接种后40 h POD比活性才开始升高,4~6 d达到高峰,峰值也较大。3类非亲和性互作PAL比活性在接种后0 h或16 h开始较明显升高,整个互作中形成3~4个较明显的峰;亲和性互作中PAL比活性一直明显下降。3类非亲和性互作外切几丁质酶比活性接种后即开始升高,基本一直保持升高趋势,在40 h前幅度较大,并形成1~3个较高的峰;亲和性互作外切几丁质酶比活性接种后即开始大幅度升高直至完全显症,48h后幅度远高于非亲和性互作。3类非亲和性互作β-1,3-葡聚糖酶比活性在24 h内开始较明显升高,在48h前形成2~3个较明显的峰;亲和性互作在接种后β-1,3-葡聚糖酶比活性即开始升高,在48h后显著高于非亲和性互作。讨论了POD、PAL、几丁质酶及β-1,3-葡聚糖酶参与水稻抗稻瘟病的可能性。     

中生菌素对水稻白叶枯病的防治机制

对不同白叶枯病抗性水稻品种用200μg/ml中生菌素55℃温汤药液浸种，自然降温，秧田3—4叶期和移栽前5d各用30μg/ml中生菌素处理后，于成株期剪叶接种白叶枯病菌。结果表明中生菌素前期处理，于成株期接种白叶枯病菌时，高抗、中等抗性和感病品种中过氧化物酶、苯丙氨酸解氨酶和多酚氧化酶3种酶活性都有不同程度的提高，且以中等抗性品种酶活提高最多，接种24和48h，3种酶活性较清水对照分别增加26．92％、26．74％、24．06％和7．09％、1．31％、1．60％。盆栽试验表明，中生菌素对中抗品种的防治效果最好，达58．4％。说明中生菌素对水稻防御酶活性的诱激作用是其防治白叶枯病的机制之一。     

丝兰属植物提取物降低鸡舍氨气浓度的效果试验

通过在21日龄的肉用仔鸡饲料中添加丝兰属植物提取物(其有效成分为丝兰皂角苷)，研究丝兰属植物提取物对降低鸡舍中氨气浓度和提高肉仔鸡生产性能的效果。试验结果表明，试验组鸡舍内氨气平均浓度为4．75mg／L，对照组鸡舍内氨气平均浓度为13．80mgl／L，试验组比对照组鸡舍内氨气平均浓度降低了9．05mg／L，经t检验，两鸡舍内氨气平均浓度差异显著(P＜0．05)，并且试验组比对照组饲料报酬提高了8.92％。     

外源氮添加对湿地土壤N_2O排放量的影响

为搞清湿地土壤驱动N2O排放的关键氮源类型,有效减少湿地N2O的排放,本文通过室内控制温湿度,用气相色谱法分析不同外源氮素对湿地N2O排放的影响。结果表明:外加氮源组总是高于对照组N2O排放量(4.4 mg·m-3)。在设定的剂量范围内,单独添加尿素或尿素与硝酸铵1∶1配合时N2O排放量呈现先增后减的单峰分布趋势,峰值分别为10.6 mg·m-3和229.0 mg·m-3;单独添加硝酸铵时N2O排放量(32.6~111.0 mg·m-3)随着氮素添加量增加呈现持续上升趋势。单独添加尿素或硝酸铵、尿素与硝酸铵1∶1配合均促进N2O的排放,但硝酸铵尿素混合添加对N2O排放量的贡献单独添加硝酸铵单独添加尿素。这为预测内蒙古高原区农牧交错带湿地氮素输入可能带来的温室效应和有效减排提供科学依据。     

白果壳遗态HAP/C复合材料对水中氨氮的吸附

为综合利用农林废弃物，以白果壳为植物模板、羟基磷灰石（HAP）为改性材料，制备了白果壳遗态HAP/C复合材料（PBGC-HAP/C-G），并通过X射线衍射仪（XRD）、傅里叶红外光谱仪（FT-IR）和扫描电镜（SEM）等对其进行了表征，同时研究了溶液pH、初始浓度、吸附剂投加量等对其去除水中氨氮的影响。结果表明，PBGC-HAP/C-G是一种大孔材料，孔径主要介于35~200 μm之间。在溶液pH=5时，吸附效果最佳；吸附剂投加量的增加有利于氨氮的去除；粒径大小不是影响吸附效果的主要因素。准二级动力学模型和Freundlich等温吸附模型能很好地描述该吸附过程，吸附过程以化学吸附为主。在氨氮初始浓度为20、50、100 mg·L^-1时，拟合计算得到的理论平衡吸附量分别为0.45、1.10、2.15 mg·g^-1，与实验测定值0.46、1.15、2.18 mg·g^-1相近，可见PBGC-HAP/C-G可用作去除氨氮的吸附剂。     

Decreasing of methanogenic activity in paddy fields via lowering ponding water temperature: A modeling investigation

Methane (CH₄) is a potent greenhouse gas and the huge CH₄ fluxes emitted from paddy fields can prejudice the eco-compatibility of rice cultivation. CH₄ production in submerged rice crops is known to be highly influenced by water temperature. Hence, lowering ponding water temperature (LPWT) could be an option to mitigate CH₄ emissions from paddy environments when it is possible either to irrigate with slightly colder water or to increase ponding water depth. However, paddy soil is a complex environment in which many processes are simultaneously influenced by temperature, leading to a difficult prediction of LPWT effects. For this reason, LPWT efficiency is here theoretically investigated with a one-dimensional process-based model that simulates the vertical and temporal dynamics of water temperature in soil and the fate of chemical compounds that influence CH₄ emissions. The model is validated with literature measured data of CH₄ emissions from a paddy field under time-variable temperature regime. Based on modeling results, LPWT appears promising since the simulated reduction of CH₄ emissions reaches about −12% and −49% for an LPWT equal to −5 °C during the ripening stage only (last 30 days of growing season, when rice is less sensitive to temperature variations) and −2 °C over the whole growing season, respectively. LPWT affects CH₄ emissions either directly (decreasing methanogenic activity), indirectly (decreasing activity of bacteria using alternative electron acceptors), or both. The encouraging results provide the theoretical ground for further laboratory and field studies aimed to investigate the LPWT feasibility in paddy environments.     

不同吸附特性的稻草生物炭对稻田氨挥发和水稻产量的影响

秸秆生物炭具有改善土壤生态环境、土壤蓄水保肥和减少温室气体排放等正效应,但其石灰效应会加大稻田氨挥发损失。为充分发挥生物炭吸铵特性,降低其石灰效应的不利影响,对不同热解温度(300、500、700℃)和酸化水平(pH值=5、7、9)稻草生物炭处理下的田面水NH_4~+-N浓度、氨挥发和水稻产量进行了研究。结果表明:偏酸性(pH值=5)、中性(p H值=7)生物炭处理在基肥期和分蘖肥期均能显著降低田面水NH_4~+-N峰值浓度(P0.05),降幅达16.90%～35.60%。全生育期稻田氨挥发损失占施氮量的15.14%～26.05%(2019年)、15.10%～19.00%(2020年)。稻田增施热解温度为700℃、酸化水平为5(p H值=5)的生物炭(C700P5)降氨效果最好,两年氨挥发分别显著降低22.93%、12.61%(P0.05)。高温热解配合偏酸性、中性生物炭(C700P5、C700P7)增产效果显著,增产率达9.92%～13.50%,结构方程模型表明,其增产原因是生物炭酸化处理降低了稻草生物炭的石灰效应,而热解温度调整提高了生物炭阳离子交换量(CationExchange Capacity,CEC),进而降低了田面水NH_4~+-N浓度和氨挥发损失,最终提高了水稻地上部氮素积累和水稻产量。研究可揭示不同热解温度和酸化水平制备的生物炭在稻田中的应用潜力,并为稻田合理施用生物炭和减少化肥施用量提供理论依据。     

区域工业发展与碳排放的脱钩关系分析——基于2006~2013年湖南的实际情况

根据湖南省“十一五”以来（2006~2013年）的工业发展和碳排放情况，分析湖南工业发展与碳排放之间的脱钩弹性、节能弹性、减排弹性，结果表明：湖南工业行业发展的过程中，较好地控制了碳排放量，但节能减排任务依然较大。因此，新常态下应以“节能、减排”为主线，深入优化产业结构，调整能源消费结构，从而确保工业可持续发展的同时，实现碳排放的合理控制。     

Isolating the effect of soil properties on agricultural soil greenhouse gas emissions under controlled conditions

Agricultural soils are important sources of greenhouse gases (GHGs). Soil properties and environmental factors have complex interactions which influence the dynamics of these GHG fluxes. Four arable and five grassland soils which represent the range of soil textures and climatic conditions of the main agricultural areas in the UK were incubated at two different moisture contents (50 or 80% water holding capacity) and with or without inorganic fertiliser application (70 kg N ha⁻¹ ammonium nitrate) over 22 days. Emissions of N₂O, CO₂ and CH₄ were measured twice per week by headspace gas sampling, and cumulative fluxes were calculated. Multiple regression modelling was carried out to determine which factors (soil mineral N, organic carbon and total nitrogen contents, C:N ratios, clay contents and pH) that best explained the variation in GHG fluxes. Clay, mineral N and soil C contents were found to be the most important explanatory variables controlling GHG fluxes in this study. However, none of the measured variables explained a significant amount of variation in CO₂ fluxes from the arable soils. The results were generally consistent with previously published work. However, N₂O emissions from the two Scottish soils were substantially more sensitive to inorganic N fertiliser application at 80% water holding capacity than the other soils, with the N₂O emissions being up to 107 times higher than the other studied soils.     

改性尿素追施对冬小麦和夏玉米季氮素挥发和淋溶的影响

以NBPT(N-丁基硫代磷酰三胺)和DMPP(3,4-二甲基吡唑磷酸盐)为复合抑制剂,利用转鼓喷涂工艺,开发出新型复合型抑制剂涂覆尿素肥料,采用扫描电镜和能谱仪分析其涂覆效果。通过田间试验系统对比评价了追施不同氮肥对调控氮素的特征效果。试验设置5个处理:(1)不施氮肥(CK);(2)农民习惯追施尿素(CU);(3)优化追施尿素(CUU);(4)优化追施抑制剂涂覆尿素(CUY1);(5)优化追施抑制剂涂覆尿素(CUY2)。在夏玉米喇叭口期、冬小麦拔节期追施氮肥后的15天内进行田间原位连续动态观测。电镜和能谱结果表明,复合抑制剂均匀涂覆于尿素表面,形成薄而致密、光滑的涂覆层,该涂覆层均匀分布有磷和硫2种元素,表明复合抑制剂与尿素已有效结合。田间试验结果表明,在同等优化施氮量下与普通尿素相比,夏玉米和冬小麦季追肥后CUY1和CUY2处理氨挥发分别降低55.19%,32.15%和52.46%,39.43%。夏玉米季追肥后,0-20 cm土层CU、CUU处理土壤硝态氮含量于第5天达到峰值,到后期已显著低于CUY1、CUY2处理,CUY2处理稳定硝态氮的效果更好。冬小麦季追肥后,0-20 cm土壤硝态氮含量CU、CUU处理分别在第5,3天达到峰值,CUY1、CUY2处理于第11天达到峰值后,硝态氮含量已显著高于相同施氮量的CUU处理。在保证产量和净收益的同时,抑制剂涂覆尿素显著降低了追施氮素的氨挥发和淋溶损失浓度,其中冬小麦季CUY1处济效益较好,夏玉米季CUY2调控氮素的效果最佳,减少向下淋溶的效果明显。