灌浆期高温胁迫对不同品种小麦蛋白组分及面团揉混特性的影响

为研究灌浆期高温胁迫对不同品种小麦蛋白组分及面团揉混特性的影响,以济麦22(JM22)和新麦26(XM26)为材料,通过灌浆初期(S1)和灌浆中期(S2)在田间搭棚进行高温胁迫处理,以未进行高温胁迫的大田小麦作对照(CK),收获后对小麦淀粉黏滞谱、蛋白质组分含量和揉混参数等进行分析。结果表明,与各自CK相比,JM22的黏滞谱参数除回复值和糊化温度降低外,其余参数均升高,XM26的黏滞谱参数除峰值时间外均降低。S1和S2使JM22的峰值黏度、低谷黏度、崩解值、最终黏度、峰值时间分别较CK提高2.81%和18.63%、7.71%和19.51%、11.88%和21.15%、1.88%和12.22%、2.45%和4.08%,且S2均大于CK和S1,S1与CK差异不显著;S1和S2使XM26的峰值黏度、低谷黏度、最终黏度、回复值分别较CK降低12.95%和31.21%、1.81%和27.18%、2.50%和22.22%、3.57%和14.39%,其中,S2、S1与CK三者之间的峰值黏度均达显著水平。与CK相比,高温胁迫后JM22的蛋白质含量降低,而XM26升高。两品种各组分蛋白含量均发生改变,S1和S2使JM22谷蛋白含量减少4.52%和6.01%,S1和S2使XM26谷蛋白增加13.66%和17.27%,不可溶蛋白增加28.95%和34.80%,谷醇比也增加。高温处理对两品种面团揉混参数值也有一定影响,S1使JM22和XM26的峰值时间、峰值高度、8 min带宽分别较各自CK显著增加8.50%和42.80%、12.20%和2.80%、26.57%和68.30%,而S2的两品种只有峰值时间同时显著增加,分别增加9.60%和28.50%。本研究结果为优质专用小麦品质提升栽培技术提供了理论基础。     

低温贮藏对猕猴桃果实成熟软化相关基因表达影响

为探究低温对果实采后成熟软化与淀粉降解的影响,以红阳猕猴桃果实为试验材料,研究在低温贮藏期间,猕猴桃果实硬度,可溶性固形物、乙烯、淀粉含量以及淀粉酶相关基因的变化。结果表明,低温贮藏能显著抑制猕猴桃果实采后成熟软化,延缓果实淀粉的降解和可溶性固形物含量的增加,维持贮藏期间果实较高的硬度。低温贮藏抑制乙烯合成关键基因AcACO1和AcACS1的表达,抑制乙烯合成。同时,低温贮藏显著抑制淀粉降解相关基因AcAMY1、AcBAM1/3、AcISA3、AcLDA1和AcDPE1的表达。在低温贮藏后期,淀粉酶相关基因AcAMY1、AcBAM1/3、AcLDA1和AcDPE1的表达与乙烯释放速率有关。综上,低温贮藏延缓猕猴桃采后成熟软化进程与淀粉降解密切相关,可能主要通过抑制乙烯合成,从而影响贮藏后期淀粉降解速率,最终延缓果实软化进程。本研究结果为猕猴桃采后低温贮藏提供了理论依据。     

Response of soil respiration to nitrogen addition in two subtropical forest types

Anthropogenic activities have increased nitrogen (N) deposition in terrestrial ecosystems, which directly and indirectly affects soil biogeochemical processes, including soil respiration. However, the effects of the increases in N availability on soil respiration are not fully understood. In this study, soil respiration was measured using an infrared gas analyzer system with soil chambers under four N treatments (0, 5, 15, and 30 g N m^-2 year^-1 as control, low N (LN), moderate N (MN), and high N (HN), respectively) in camphor tree and slash pine forests in subtropical China. Results showed that soil respiration rates decreased by 37% in the camphor tree forest and 27% in the slash pine forest on average on an annual base, respectively, in the N-fertilized treatments when compared with the control. No significant differences were found in the soil respiration rate among the LN, MN, and HN treatments in both forest types as these fertilized plots reached an adequate N content zone. In addition, soil microbial biomass carbon (C) content and fine root biomass declined in N-treated plots compared to the control. Our results indicated that elevated N deposition might alter the tree growth pattern, C partitioning, and microbial activity, which further affect soil C sequestration by reducing soil respiration in subtropical forests of China.     

储料竖向压力对粮仓中小麦粮堆湿热传递的影响

粮仓中存在压力场、温度场和湿度场等多物理场,为了得出各物理因子共同影响下的粮堆内湿热传递规律,该研究利用自行研制的粮堆多场耦合试验装置,针对仓内小麦粮堆单元体,研究在高温边界38.5℃、低温边界5.2℃,初始粮温25.8℃,竖向压力分别为50、100、150 kPa条件下小麦粮堆湿热传递情况。试验结果表明:竖向压力增加,粮堆孔隙率减小,热量通过粮食籽粒间传导增加,传递速率加快,竖向压力从50 kPa增大至150 k Pa,粮温较入仓时下降约0.5~1.3℃,温度梯度变化率达8.7%,不同压力下粮堆高温区面积随储藏时间呈幂函数减小。粮堆内湿空气在边界处累积至峰值时会有部分湿空气向粮堆内迁移。粮堆中部与靠近低温边界温差大于6.3℃时,粮堆内湿空气扩散加快,粮堆中部平均相对湿度下降速率随竖向压力增加而加快。研究结果可为散装粮堆多场耦合研究提供理论支持。     

滴灌条件下水土温度对覆砂土壤水热运移影响的数值模拟

为探究滴灌条件下水温与土温对覆砂土壤水热运移规律的影响,基于HYDRUS-2D构建了不同水土温度土壤水热运移数值模型,模拟分析了不同水土温度对覆砂土壤水分、温度动态变化的影响。结果表明:灌溉水温对土壤水热分布影响显著,随着温度升高,土壤湿润体内含水率减小,表现为35℃水温20℃水温5℃水温,灌溉水温对土壤剖面温度分布也有较大影响,表层0—15 cm范围内温度变化了5～10℃。相同水温条件下,随着土壤温度升高,土壤饱和导水率增大,湿润土体内体积含水率减小,表现为30℃土壤温度15℃土壤温度5℃土壤温度。滴灌水平和垂直湿润锋运移距离随温度升高而增大,湿润锋运移距离与时间符合幂函数F=at~b,决定系数R~2介于0.977 4～0.999 6,并建立了水平和垂直湿润锋运移距离与入渗时间和温度的关系模型。以期为西北干旱地区砂石覆盖生态农业的合理补灌提供理论指导。     

气候变暖背景下河南省夏玉米花期高温灾害风险预估

为预估未来气候变暖背景下夏玉米花期高温灾害风险,根据河南省19个农业气象观测站夏玉米抽雄期常年观测资料和未来RCPs(representativeconcentrationpathways)气候变化情景数据,构建夏玉米花期高温风险评价指标,开展河南省夏玉米花期高温灾害时空特征及风险演变分析。其中RCPs气候情景数据包括基准气候条件(1951—2005年, RCP-rf)和未来(2006—2050年)RCP 4.5(中)、RCP 8.5(高)两种浓度路径数据。以抽雄普遍期及之后7d确定为夏玉米花期,并内插匹配气候情景格点数据。以花期最高气温≥32℃和≥35℃作为轻度和重度高温灾害发生阈值,根据轻、重度夏玉米花期高温发生频率和高温积害,建立风险评价指标并分级。结果表明, RCP-rf情景下全省夏玉米花期高温发生频率在20.5%～81.0%(≥32℃)和3.9%～51.9%(≥35℃)。与基准条件相比,≥32℃高温发生频率增加9.1%(RCP4.5)和11.0%(RCP8.5),≥35℃高温发生频率增加8.7%(RCP4.5)和8.3%(RCP8.5)。RCP-rf情景下全省夏玉米花期高温积害在48.5～200.9℃·d(≥32℃)和9.8～138.5℃·d(≥35℃)。与基准条件相比,≥32℃高温积害增加25.4℃·d (RCP 4.5)和25.6℃·d (RCP 8.5),≥35℃高温积害增加25.8℃·d (RCP 4.5)和31.4℃·d (RCP 8.5)。由综合风险分析可知, RCP-rf情景下夏玉米花期高温灾害高值风险区主要分布在新乡、郑州、许昌、漯河、周口及其以东以北的地区(商丘除外),约占夏玉米主栽区面积的30.1%;RCP4.5情景下高值风险区扩大至洛阳和南阳以东的大部分地区,约占夏玉米主栽区面积的63.4%; RCP 8.5情景下高值风险区面积进一步向西扩大,约占夏玉米主栽区面积的占76.3%。     

The use of the hand-held infrared thermometer as an early detection tool for exertional heat illness in Thoroughbred racehorses: A study at racetracks in eastern Australia

Thoroughbred racehorses perform exercise at maximal intensities and typically display a hyperthermic exercise response, which can drive core body temperature to critical levels. Despite extremely efficient thermoregulatory mechanisms, certain weather conditions may affect the horse’s ability to cool and result in a syndrome referred to as exertional heat illness (EHI). This is characterised by central nervous system dysfunction, as well as cytotoxic effects of heat on cells, which can produce deleterious consequences. Early detection of exertional heat illness (EHI) in Thoroughbred racehorses can be difficult because signs are often vague and the measurement of rectal temperature as an indicator of hyperthermia is not practical. Best practice in the treatment of EHI in horses, as in human subjects, centres on early detection, rapid assessment and aggressive cooling. Research in human subjects has shown that EHI is manageable when recognised early and appropriate treatment provided. The aim of this study was to investigate the measurement of skin surface temperature (SST) by an infrared thermometer as an aid in the early detection of EHI. A skin surface temperature ≥39°C in the immediate postrace period is considered to be hot. It reflects the interaction of exercise-related metabolic heat production, physiological adjustments to the skin surface such as vasodilation and sweating, together with the effect of high ambient temperature. Most importantly, high SST is associated with a reduced core-to-skin temperature difference, which retards heat transfer from the deep body tissues to the skin and can hinder heat dissipation. Identification of horses with high SSTs can prioritise them for rapid cooling and curtail possible progression to EHI.     

Short-term spatiotemporal variation of soil CO2 emission,temperature, moisture and aeration in sugarcane field reform areas under the influence of precipitation events

Soil CO₂ emission (FCO₂) in agricultural areas results from the interaction of different factors such as climate and soil conditions. Our objective was to investigate the spatiotemporal variation of FCO₂, temperature (T_soil), moisture (M_soil) and air-filled pore space (AFPS), as well as their interactions, during the sugarcane field reform. The study was conducted on a 90 × 90 m sampling grid with 100 points at 10 m spacings. Ten assessments of FCO₂, T_soil and M_soil were carried out at each point over a 28-day period. The greatest mean values of FCO₂ (0.74 g m⁻² hr⁻¹) and M_soil (31.7%) were obtained on Julian day 276, 2013, being associated with precipitation events at the study site. Also, the smallest values of AFPS (19.17%) and T_soil (20.90°C) were observed on the same day. The spatial variability of FCO₂, T_soil, M_soil and AFPS was best described by an adjusted spherical model, although an exponential model better fitted some results. The spatial pattern of all soil attributes showed little temporal persistency, indicating a high complexity for FCO₂ during precipitation. Correlation maps assisted in identifying regions where M_soil and AFPS better controlled the emission process and where T_soil was important. A major challenge for world agriculture is to increase the efficiency of conventional soil management practices. We highlight the importance of the spatial pattern of soil properties that directly influence the CO₂ emission dynamics. Future mitigation actions should involve less intense tillage and ensure homogeneous applications of soil inputs, thereby reducing production costs and the contribution of these activities to CO₂ emissions during the sugarcane field reform.     

气候变化对宝鸡地区植被覆盖时空演变的影响

植被覆盖变化及其对气候因子的响应研究是一个长期、复杂的动态过程，本研究基于MODIS NDVI数据和宝鸡气象局11个气象站点的气候因子（气温、降水量）数据，运用趋势和相关分析法等探讨宝鸡地区近13年植被覆盖的时空变化规律及与年均温和年降水量之间的相互关系，为区域农业发展和生态文明建设工作提供了理论支撑。结果表明：（1）宝鸡地区近13a年均NDVI以0.025/10 a的速度上升，较快于三北防护林工程区1982—2006年植被覆盖的增速(0.007/10 a)，且出现2001—2002年、2003—2004年两次高恢复期；（2）多年NDVI高值区集中于太白河和湑水河之间的太白县南部地区。千河沿岸及渭河流域宝鸡段的宝鸡市、宝鸡县、凤翔、岐山南北沿岸的“带状”地区，植被覆盖最低；（3）全区植被覆盖与气温较显著正相关像元占15.016% (P<0.05)，与降水量较显著正相关像元占16.872% (P<0.05)，相关性均较好。     

青藏高原东部强降温过程阈值的探讨及其气候特征

为解决青藏高原东部强降温的气象预报和服务问题,利用青藏高原东北部68个气象站1961-2017年逐日最低气温数据,辅以趋势分析及相关分析等方法,本文探讨了近57年青藏高原东北部强降温的阈值及气候特征,并利用NECP/NCAR(2.5°×2.5°)海温场、高度场建立了预报诊断模型。研究发现 (1) 应用改进的强降温指标统计寒潮发生的特征更符合高原实际情况。(2)受地形地貌及山脉阻挡的影响,青藏高原东部强降温次数的地域分布存在明显差异,海拔较高的山区和东部地区强降温次数明显多于盆地。南部山区24h寒潮发生的次数多于48h、72h。(3)近57年区域寒潮频次总体呈下降趋势,南部和北部的降速分别为-0.5次/10a、-0.4次/10a,并通过显著性检验；西北部盆地区降速分别为-0.1次/10a,未通过显著性检验。(4)高冷空气的移动路径是强降温预测的关键信号。研究结果为青藏高原相关部门开展农牧业资源的和旅游资源的相关决策服务提供科学依据。