基于灰色关联度分析气候因素对江西省松材线虫病的影响

为分析不同气候因素对松材线虫Bursaphelenchus xylophilus引起的松材线虫病的影响程度,本文以江西省全南县(代表赣南,松墨天牛一年2代)和德兴市(代表赣北,松墨天牛一年1代)遭受松材线虫病危害的马尾松林生态系统为研究对象,获取2018年-2021年松材线虫病普查数据和1990年-2021年的主要气象因子数据,结合滑动平均法和灰色关联度分析法比较分析两地的气候差异和疫情年间气候变化对松材线虫病发病面积的影响。结果显示:除德兴市的年均相对湿度和年降水量与历年平均值相比有所降低外,两地其他气象因子均呈上升趋势;灰色关联度分析表明,年均最高气温和年均风速是影响赣南松材线虫疫情的重要气象因子,年均最高气温和年降水量是影响赣北松材线虫疫情的重要气象因子;气温升高促进松材线虫和其媒介昆虫的生长繁殖与活动,风速升高可使媒介昆虫远距离传播松材线虫,降水量减少可降低松材线虫和媒介昆虫染病死亡几率。赣南赣北气候的整体变化趋势都有利于松材线虫病的扩散蔓延。     

限水灌溉对冬小麦灌浆期旗叶叶绿素荧光动力学参数及产量的影响

在池栽、遮雨条件下,利用植物效能分析仪研究了减少灌水次数对豫麦50灌浆期旗叶叶绿素荧光动力学参数及产量的影响.结果表明,不同灌水处理小麦旗叶叶绿素含量和Tm值开花后均较高,然后逐渐降低;Fv/Fo、Fv/Fm在灌浆中、前期差异不大,而在灌浆末期迅速降低.全生育期不灌水处理在灌浆期旗叶叶绿素含量、Tm、Fv/Fo和Fv/Fm较低,而拔节期灌1水处理则较高.减少灌水次数会降低籽粒产量和田间耗水量,而提高了水分利用效率.     

Soil surface roughness change and its effect on runoff and erosion on the Loess Plateau of China

As an important parameter in the soil erosion model, soil surface roughness（SSR） is used to quantitatively describe the micro-relief on agricultural land. SSR has been extensively studied both experimentally and theoretically; however, no studies have focused on understanding SSR on the Loess Plateau of China. This study investigated changes in SSR for three different tillage practices on the Loess Plateau of China and the effects of SSR on runoff and erosion yield during simulated rainfall. The tillage practices used were zero tillage（ZT）, shallow hoeing（SH） and contour ploughing（CP）. Two rainfall intensities were applied, and three stages of water erosion processes（splash erosion（I）, sheet erosion（II） and rill erosion（III）） were analyzed for each rainfall intensity. The chain method was used to measure changes in SSR both initially and after each stage of rainfall. A splash board was used to measure the splash erosion at stage I. Runoff and sediment data were collected continuously at 2-min intervals during rainfall erosion stages II and III. We found that SSR of the tilled surfaces ranged from 1.0% to 21.9% under the three tillage practices, and the order of the initial SSR for the three treatments was ZT〈SH〈CP. For the ZT treatment, SSR increased slightly from stage I to III, whereas for the SH and CP treatments, SSR decreased by 44.5% and 61.5% after the three water erosion stages, respectively, and the greatest reduction in SSR occurred in stage I. Regression analysis showed that the changes in SSR with increasing cumulative rainfall could be described by a power function（R2〉0.49） for the ZT, SH and CP treatments. The runoff initiation time was longer in the SH and CP treatments than in the ZT treatment. There were no significant differences in the total runoff yields among the ZT, SH and CP treatments. Sediment loss was significantly smaller（P〈0.05） in the SH and CP treatments than in the ZT treatment.