Impact of climate change on maize yield in China from 1979 to 2016

Climate change severely impacts agricultural production, which jeopardizes food security. China is the second largest maize producer in the world and also the largest consumer of maize. Analyzing the impact of climate change on maize yields can provide effective guidance to national and international economics and politics. Panel models are unable to determine the group-wise heteroscedasticity, cross-sectional correlation and autocorrelation of datasets, therefore we adopted the feasible generalized least square(FGLS) model to evaluate the impact of climate change on maize yields in China from 1979–2016 and got the following results:(1) During the 1979–2016 period, increases in temperature negatively impacted the maize yield of China. For every 1°C increase in temperature, the maize yield was reduced by 5.19 kg 667 m–2(1.7%). Precipitation increased only marginally during this time, and therefore its impact on the maize yield was negligible. For every 1 mm increase in precipitation, the maize yield increased by an insignificant amount of 0.043 kg 667 m–2(0.014%).(2) The impacts of climate change on maize yield differ spatially, with more significant impacts experienced in southern China. In this region, a 1°C increase in temperature resulted in a 7.49 kg 667 m–2 decrease in the maize yield, while the impact of temperature on the maize yield in northern China was insignificant. For every 1 mm increase in precipitation, the maize yield increased by 0.013 kg 667 m–2 in southern China and 0.066 kg 667 m–2 in northern China.(3) The resilience of the maize crop to climate change is strong. The marginal effect of temperature in both southern and northern China during the 1990–2016 period was smaller than that for the 1979–2016 period.     

基于土地利用调查成果的草原资源监测技术研究

草原是我国陆地生态系统的重要主体,也是生态文明建设的主战场之一.但草原资源本底不清,限制了草原的科学管理.按照牧区、半牧区、林区草原资源的差异性,分别选择典型县域进行案例分析.结果表明,由于草地认定标准差异、资源自身空间上的重叠、精度差异等方面原因,三调初步成果与原有的调查资料草地面积总量和空间分布均存在不同程度的差异;国土三调初步成果的图斑区划和属性因子不能满足草原资源经营管理的需求,应在三调的基础上进行经营区划和调查;草班和小班的区划要满足不同区域草原资源管理和经营的需要,调查内容包括类型、数量、质量、结构和功能等5个方面.     

桉树不同成熟度叶片营养元素内循环特征

揭示桉树人工林不同成熟度的叶片器官所需营养元素变化以及土壤肥力对其影响,对于桉树营林和科学施肥具有重要的生产指导意义。选取广西隆安县小林镇和田东县思林镇的桉树2代萌芽林作为研究对象,测定两个人工林嫩叶、成熟叶、黄叶的C、N、P、K、B、Ca、Mg以及土壤C、N、P、K、Ca、Mg元素含量,并进行相关分析。结果表明,植物叶片的N、P、K、Mg营养元素转移规律是黄叶向成熟叶和嫩叶转移,但C、Ca、B营养元素则是随着叶片的生长发育逐渐积累,黄叶中含量最高,说明施肥时应关注Ca、B元素的持续和有效供给。两片人工林都表现出类似的规律,说明土壤肥力的差异不影响桉树人工林叶片营养元素的内循环规律。桉树嫩叶营养元素含量及其生态化学计量比学特征具有与成熟叶和黄叶不同的表征,在营养物质研究中应予以足够重视。     

江西省数字农业发展现状、问题与建议

数字农业的发展对于农业现代化转型升级具有重要意义。根据江西省县域数字农业相关数据和文献资料,分析江西省数字农业发展现状,指出目前江西省数字农业发展存在数据服务配套不完善、小农户应用困难以及法律法规政策建设相对落后等问题,提出应加强数字农业信息服务支持力度、培育新型农业经营主体,以及强化政策顶层设计等建议。     

响应面优化早花忍冬组培苗增殖培养条件

本试验以早花忍冬组培苗的茎段为试验材料,采用Box-Behnken响应面设计法优化早花忍冬茎段继代培养的条件,为早花忍冬组培离体快繁体系建立提供了参考依据.通过单因素试验法确定激素的添加范围,通过响应面优化得到最佳的增殖培养基.结果表明:激素种类对早花忍冬组培苗茎段继代培养的影响顺序依次为:6-BA＞IAA＞IBA,并且在6-BA浓度为1.9 mg/L、IBA浓度为0.76 mg/L、IAA浓度为0.27 mg/L时,茎段继代培养的增殖系数为7.66,与方程预测值相接近.     

稻瘟病菌CAAX蛋白酶MoRce1的功能研究

 蛋白质的翻译后异戊烯化修饰(CAAX修饰)能够介导真核生物中许多重要蛋白质的亚细胞定位以及蛋白与蛋白间的相互作用。稻瘟病菌(Magnaporthe oryzae)引致的稻瘟病是水稻最重要病害之一,造成全球水稻严重减产。为深入了解稻瘟病菌致病机理,更好地防控稻瘟病,我们研究了异戊烯修饰是否影响稻瘟病菌的生长发育和致病性。首先从稻瘟病菌基因组数据库中鉴定到一个稻瘟病菌的异戊烯蛋白酶MoRce1,同源比对发现MoRce1保守结构域在各物种之间变化较大,猜测在不同物种中该蛋白可能出现了功能分化。经同源重组方法敲除MoRCE1基因,发现MoRCE1缺失突变体在胁迫培养条件下细胞壁完整性明显缺陷,但是对营养生长、产孢、萌发以及致病性没有明显影响,说明MoRce1蛋白可能通过参与稻瘟病菌细胞壁合成相关蛋白的异戊烯化修饰进而影响该菌细胞壁的完整性,其具体机制还有待深入研究。     

光照对箭筈豌豆及其子代生长和繁殖特性的影响

光照不仅会影响植物自身的生长,也可能会对其子代的生长具有潜在作用。以箭筈豌豆品种兰箭1号和兰箭3号为材料,分析遮荫和自然光照下箭筈豌豆及其子代的生长特性。结果表明:光照对箭筈豌豆生长和繁殖特性的影响因基因型而异。与光照条件相比,遮荫显著降低兰箭1号生物量及茎叶比,但对繁殖分配的比例影响不显著。与此相反,遮荫对兰箭3号的生长与繁殖无显著影响;母本光照环境对箭筈豌豆子代生长特性具有一定程度的影响,且这种影响因子代植株生长的光照环境而异。当子代在遮荫环境下,母本环境显著影响兰箭1号分枝数、地上生物量、总生物量、地上/地下生物量以及兰箭3号的分枝数。但当子代在光照环境下生长时,除兰箭3号分枝数外,其他生长特性均不受母本环境影响。     

天津春稻和麦茬稻品质特性比较

以天津市培育的优质小站稻品种津川1号和隆优619为供试材料,分析了春稻和麦茬稻品质特性的差异。结果表明,津川1号作麦茬稻的整精米率明显低于作春稻,而垩白粒率显著高于春稻;津川1号麦茬稻的蛋白质含量明显偏高,食味值显著低于春稻;隆优619作春稻和麦茬稻无论在外观、加工、食味还是营养品质方面均无显著差异,是较理想的麦茬连作品种。     

岩溶流域典型农业区水体氢氧同位素的空间异质性及形成机制

分别于平水期和枯水期采集了花溪河流域典型农业区地表水和地下水样品。利用氢氧同位素示踪技术,结合土地利用类型对研究区不同水体的补给来源、季节变化及主要影响过程进行了分析,并对不同水体氢氧同位素值进行了空间插值分析,同时对其形成机制进行了分析,阐明了不同土地利用类型影响下的主要水文过程。结果表明:(1)研究区不同水体的主要补给来源为当地大气降水,月亮湖水库受蒸发作用影响明显,地表水和地下水的δD和δ~(18)O整体上呈现平水期高于枯水期的特征。(2)地下水的δD和δ~(18)O在枯水期与平水期均呈现明显的空间分异性特征,西部水田/水库集中区富集,东部旱地集中区贫化,土地利用对研究区环境水文过程影响明显。该研究结果有助于了解不同土地利用方式下地表水对地下水的影响,为流域管理提供科学依据。     

Impact of grassland contract policy on soil organic carbon losses from alpine grassland on the Qinghai–Tibetan Plateau

Carbon storage in the soils on the Qinghai–Tibetan Plateau plays a very important role in the global carbon budget. In the 1990s, a policy of contracting collective grasslands to smaller units was implemented, resulting in a change from the traditional collective grassland management to two new management patterns: a multi‐household management pattern (MMP: grassland shared by several households without enclosures) and a single‐household management pattern (SMP: grassland enclosed and used by only one household). In 2016, 50 MMP and 54 SMP winter pastures on the Qinghai–Tibetan Plateau were sampled to assess the differences in soil organic carbon (SOC) between the two management patterns. Results showed that average SOC was significantly greater under MMP than under SMP, with an estimated 0.41 Mg C/ha/yr lost due to SMP following the new grassland contract. Based on the government's grassland policy, four grassland utilization scenarios were developed for both summer and winter pastures. We found that if the grassland were managed under SMP, likely C losses ranged between 0.31 × 10⁷ and 6.15 × 10⁷ Mg C/yr across the Qinghai–Tibetan Plateau relative to MMP, which more closely resembles pre‐1990s grassland management. Previous estimates of C losses have only considered land use change (with cover change) and ignored the impacts driven by land management pattern changes (without cover change). The new data suggest that C losses from the Qinghai–Tibetan Plateau are greater than previously estimated, and therefore that the grassland contract policy should be reviewed and SMP households should be encouraged to reunite into the MMP. These findings have potential implications for land management strategies not only on the Qinghai–Tibetan Plateau but also other grazing regions globally where such practices may exist.