江西省水稻蓄雨间歇灌溉模式初探

【目的】探索水稻蓄雨间歇灌溉模式节水减排效益。【方法】以鄱阳湖区双季早晚稻为试验材料,采用大田和测坑试验,研究了水稻蓄雨间歇灌溉模式对灌溉定额、排水定额、降雨有效利用率、产量、稻田水分生产率,以及氮、磷排放量的影响,并与间歇灌溉和常规淹水灌溉试验进行了分析比较。【结果】与淹水灌溉、间歇灌溉相比,蓄雨间歇灌溉灌排水量、灌排次数明显减少。双季早晚稻年平均灌水量分别减少975m^3/hm^2和1251m^3/hm^2,年平均灌水次数分别减少8次和7.5次;年平均排水量分别减少729 m^3/hm^2和893 m^3/hm^2,年平均排水次数分别减少5.8次和3.1次;蓄雨间歇灌溉降雨有效利用率明显提高。早稻降雨利用率分别提高12.40%和9.14%,晚稻分别提高6.84%和6.42%;蓄雨间歇灌溉模式下,双季早晚稻总氮排放量年平均减排7.64 kg/hm^2和3.12 kg/hm^2,减排幅度34.93%和14.26%;双季早晚稻总磷排放量0.180kg/hm^2和0.095kg/hm^2,减排幅度37.25%和70.59%。【结论】蓄雨间歇灌溉模式具有明显的节水、减排和提高降雨有效利用率的效果,在我国南方多雨地区具有较强的推广应用空间。     

荔枝果肉热泵干燥及其储藏特性研究

为了探讨荔枝果肉热泵干燥特性及储藏过程中一些品质指标的变化规律，将去皮去核后的果肉进行热泵干燥，测定其干燥特性及储藏过程中色泽、褐变度、总酸、糖组分、质构及微生物指标的变化。结果表明：荔枝果肉在60 ℃下热泵干燥2 h，干燥速度升至最大值后进入降速干燥阶段，干燥过程中，亮度L*值变化不大，a*值和b*值显著增大；干燥18~20 h，样品的水分含量达25%左右、颜色呈金黄色；不同水分含量的荔枝果肉干在储藏过程中，L*值、a*值和b*值下降，果肉发生褐变，总酸含量呈上升趋势，果糖、葡萄糖和蔗糖呈减少趋势；水分含量35%的样品储藏180 d褐变明显；荔枝果干的硬度和咀嚼性在储藏后期明显增大，黏着性变化不显著。采用热泵干燥荔枝果肉，25%水分含量的样品品质和储藏性较佳。     

8℃相变蓄冷技术

指出了自“十二五”规划以来,可持续发展和能源结构转型成为我国政府工作的重中之重,合理利用能源为人类社会创造更加美好的现代生活已经成为社会的共识。蓄冷技术能够按需实现能量的存储和释放,从宏观上起到“移峰填谷”平衡电网的作用;我国电力系统实行分时计价政策,从微观上可以利用峰谷电价差为用户节省制冷系统的运行费用。8℃相变蓄冷技术兼备了传统水蓄冷和冰蓄冷的优点,具有蓄冷密度大、系统简单的突出优点,是当前蓄冷技术研究和应用的前沿方向,市场前景十分广阔。     

北方草地及农牧交错区草地植被碳储量及其影响因素

【目的】 草地生态系统在全球碳平衡中有重要的意义,草地植被碳库及其变化机制研究是植被生态学的重要命题。本文研究北方草地和农牧交错区草地植被碳密度及其空间格局,解析不同区域草地植被碳密度的关键影响因素,分析了气候、土壤、放牧等因素对地上地下植被碳库的相对贡献。【方法】 基于2002—2009年北方草地及农牧交错带草地植被调查数据,结合同期MODIS/NDVI遥感影像和1﹕100万草地类型图,建立了我国主要草地类型的生物量估算模型;整合野外考察数据和前人研究结果,探讨了研究区地上地下生物碳库及其空间格局;基于研究区255个县级行政单元,分析了不同类型草地植被碳库与气候要素、土壤要素及家畜承载量的关系,应用一般线性模型（GLM）解析了不同影响因素对草地碳密度的相对贡献。【结果】 （1）北方草地与农牧交错区草地地上平均生物碳密度为36.9 g C·m^-2,地下生物碳密度为362.9 g C·m^-2,地下生物碳密度高于地上10倍,均呈从东到西递减的趋势,频率分布图基本服从对数正态分布,不同草地类型的生物碳密度存在明显差异;（2）整个研究区及草原亚区、荒漠亚区、农牧交错亚区内,地上生物量与年降水量（MAP）呈极显著正相关、与年均气温（MAT）均呈极显著负相关,与土壤黏粒含量（Clay%）呈显著正相关、与土壤砂粒含量（Sand%）呈显著负相关,整个研究区家畜承载量与草地地上生物量之间呈极显著正相关;（3）一般线性模型（GLM）分析结果表明,年平均降水量（MAP）、年均气温（MAT）、土壤黏粒含量（Clay%）、放牧强度对地上生物量空间变异的解释率分别达到29.6%（P<0.001）、5.8%（P<0.001）、0.8%（P<0.05）、1.3%（P<0.001）;地下生物量的空间变异主要来自于年降水量（MAP）、年均气温（MAT）、土壤砂粒含量（Sand%）,对方差的解释率分别达到12.1%（P<0.001）、6.8%（P<0.001）、1.9%（P<0.005）,放牧强度没有明显贡献。【结论】 气候条件尤其是年降水量是草地生物量碳库的主要影响因素,但对地上生物量影响更为明显;土壤质地对植被生物碳库也有显著贡献,尤其对地下生物量的影响更加显著;放牧强度只能解释地上生物量变化的1.3%、对地下生物量没有显著贡献,这一发现意味着气候对生物量碳库的贡献远大于放牧影响。     

Soil organic carbon fractions and humic substances are affected by land uses of Caatinga forest in Brazil

Caatinga is a Brazilian dry ecosystem that occupies around 1 million km² and is one of the largest tropical dry forests of the world. About 46% of the area that was originally covered has been deforested. Land use can cause pronounced reduction in soil carbon stocks that play a major role in the global carbon cycle. The objective of this study was to improve our understanding of the effect of land use on oxidizable carbon fractions, total carbon stocks and humic substances in different layers of soil in a Brazilian semi-arid region. We analyzed soils from tropical dry forest (TDF), forest succession with Anadenanthera falcata (ANA), with Tabebuia alba (TAB), secondary scrubby regeneration (SCR), and non-irrigated maize (MS). Forests showed larger fractions of more labile carbon, except for TDF. The most recalcitrant fraction of carbon stock, humin fraction stock, with the different land use decreased by 38–53% compared to TDF. Oxidizable carbon fractions, carbon stocks, and humic fraction stocks were able to differentiate the successional land uses and agricultural cover from TDF, mainly in the 0–5?cm layer. Our results show that changes in land use, especially with ANA forest succession, showed a larger labile carbon fraction, indicating easy decomposition and loss. Our results provide an alternative tool for the management of deforested areas in tropical dry caatinga ecosystems. This would contribute to the conservation of dry forest systems and could serve as guideline for sustainable management of agriculturally impacted caatinga areas.     

Effects of different tillage and straw retention practices on soil aggregates and carbon and nitrogen sequestration in soils of the northwestern China

Soil tillage and straw retention in dryland areas may affect the soil aggregates and the distribution of total organic carbon. The aims of this study were to establish how different tillage and straw retention practices affect the soil aggregates and soil organic carbon (SOC) and total nitrogen (TN) contents in the aggregate fractions based on a long-term (approximately 15 years) field experimentin the semi-arid western Loess Plateau, northwestern China. The experiment included four soil treatments, i.e., conventional tillage with straw removed (T), conventional tillage with straw incorporated (TS), no tillage with straw removed (NT) and no tillage with straw retention (NTS), which were arranged in a complete randomized block design. The wet-sieving method was used to separate four size fractions of aggregates, namely, large macroaggregates (LA, >2000 μm), small macroaggregates (SA, 250-2000 μm), microaggregates (MA, 53-250 μm), and silt and clay (SC, <53 μm). Compared to the conventional tillage practices (including T and TS treatments), the percentages of the macroaggregate fractions (LA and SA) under the conservation tillage practices (including NT and NTS treatments) were increased by 41.2%-56.6%, with the NTS treatment having the greatest effect. For soil layers of 0-5, 5-10 and 10-30 cm, values of the mean weight diameter (MWD) under the TS and NTS treatments were 10.68%, 13.83% and 17.65%, respectively. They were 18.45%, 19.15% and 14.12% higher than those under the T treatment, respectively. The maximum contents of the aggregate-associated SOC and TN were detected in the SA fraction, with the greatest effect being observed for the NTS treatment. The SOC and TN contents were significantly higher under the NTS and TS treatments than under the T treatment. Also, the increases in SOC and TN levels were much higher in the straw-retention plots than in the straw-removed plots. The macroaggregates (including LA and SA fractions) were the major pools for SOC and TN, regardless of tillage practices, storing 3.25-6.81 g C/kg soil and 0.34-0.62 g N/kg soil. Based on the above results, we recommend the NTS treatment as the best option to boost soil aggregates and to reinforce carbon and nitrogen sequestration in soils in the semi-arid western Loess Plateau of northwestern China.     

不同浓度1-MCP对柿果保鲜效果研究及灰色关联性分析

以恭城月柿为试材，采用精准相温（-0.5±0.3）℃结合不同浓度（0（CK）、1、3、5 ?滋L/L）1-甲基环丙烯（1-MCP）的处理方式，探索1-MCP最佳处理浓度及对柿果保鲜效果的影响。结果表明，不同浓度1-MCP处理均可保持柿果的感官品质、色泽及抗坏血酸（VC）含量，降低乙烯呼吸速率和丙二醛含量，从而达到延长贮藏期和维持柿果品质的目的，且随着贮藏时间的延长，保鲜效果更加显著，但是对可滴定酸（TA）含量及呼吸强度并无显著影响。灰色关联分析可知，4个处理的关联度分别为0.566、0.885、0.654、0.722，按大小排序为1 ?滋L/L 1-MCP＞5 ?滋L/L 1-MCP＞3 ?滋L/L 1-MCP＞CK，说明采用浓度为1 ?滋L/L 1-MCP处理柿果能够具有最佳贮藏效果，5 ?滋L/L 1-MCP次之，3 ?滋L/L 1-MCP效果较差。     

灌浆温度和氮肥及其互作效应对稻米贮藏蛋白组分的影响

灌浆结实期温度与氮肥施用量是影响稻米品质的两个重要生态因子,尤其是与稻米蛋白含量及米饭食味关系密切。本文以多个水稻主栽品种为材料,通迆灌浆结实期的人工控温试验、大田长期定位点的施氮处理试验和盆栽条件下的温氮两因素复合处理试验,探讨了水稻灌浆结实期温度对稻米贮藏蛋白含量与组分影响及其有别于氮肥处理效应的差异觃律,幵分析了温度与氮肥两个因素对稻米贮藏蛋白及其组分影响的交互作用特点。结果表明,高温胁迫和增施氮肥均引起水稻籽粒总蛋白及其谷蛋白组分含量(%)的显著增加,但两者对稻米醇溶蛋白影响却存在明显差别。其中,高温处理引起醇溶蛋白含量显著下降,提高稻米谷蛋白/醇溶蛋白比值,而增施氮肥引起稻米谷蛋白和醇溶蛋白含量明显增加,但对谷蛋白/醇溶蛋白比值与贮藏蛋白各亚基的组成比例影响相对较小。在高温处理下,谷蛋白的57kD前体亚基组分含量有所提高,而37kD酸性亚基和22kD碱性亚基随温度处理的差异变化却因品种而异,且高温处理对水稻籽粒蛋白绝对含量(mg grain~(–1))的影响程度也进没有其对蛋白相对含量(%)的影响明显。高氮×高温处理组合对稻米总蛋白与谷蛋白含量的影响程度显著大于单一高温或高氮处理,但在高氮水平下由高温引起稻米醇溶蛋白含量的下降幅度却小于其低氮对照,有利于稻米醇溶蛋白含量在不同温度处理下的相对稳定。     

免耕对土壤微生物量碳影响的Meta分析

为综合分析免耕(NT)对土壤微生物碳含量的影响程度,以常规耕作(CT)为对照,收集国内外关于免耕对土壤微生物碳研究已公开发表的41篇文献的田间试验数据162组,采用Meta数据整合分析方法,定量分析中国不同区域、气候类型和试验年限下,免耕对于中国农田土壤微生物碳含量的影响。结果表明,与常规耕作相比,免耕能显著提高土壤微生物碳的含量,免耕-常规耕作(NT-CT)的加权均数差值(WMD)为49.29 mg·kg^-1;免耕对土壤中微生物碳含量的影响存在区域差异性,西南地区WMD最大,湿润区(年降雨量>800 mm)免耕对土壤微生物碳含量的正效应最显著;年均温度10~15℃和年均温度>15℃时,免耕土壤中微生物碳含量显著高于常规耕作,且随着温度的升高而增加;免耕年限能够显著影响土壤微生物碳含量,以长期免耕(免耕年限≥8 a)效果最佳。综上,免耕对土壤微生物碳的增加效应存在区域特征,以西南地区最高,随着区域水热条件、免耕年限的不同有所差异,免耕措施的采用应该根据区域特点因地制宜。本研究结果为免耕的区域性合理利用提供了参考依据。