Effects of elevated temperature on soil respiration in a coastal wetland during the non- growing season in the Yellow River Delta,China

Aims Winter soil respiration plays a crucial role in terrestrial carbon cycle, which could lose carbon gained in the growing season. With global warming, the average near-surface air temperatures will rise by 0.3 to 4.8 °C. Winter is expected to be warmer obviously than other seasons. Thus, the elevated temperature can significantly affect soil respiration. The coastal wetland has shallow underground water level and is affected by the fresh water and salt water. Elevated temperature can cause the increase of soil salinity, and as a result high salinity can limit soil respiration. Our objectives were to determine the diurnal and seasonal dynamics of soil respiration in a coastal wetland during the non-growing season, and to explore the responses of soil respiration to environmental factors, especially soil temperature and salinity.
Methods A manipulative warming experiment was conducted in a costal wetland in the Yellow River Delta using the infrared heaters. A complete random block design with two treatments, including control and warming, and each treatment was replicated each treatment four times. Soil respiration was measured twice a month during the non-growing season by a LI-8100 soil CO₂ efflux system. The measurements were taken every 2 h for 24 h at clear days. During each soil respiration measurement, soil environmental parameters were determined simultaneously, including soil temperature, moisture and salinity.
Important findings The diurnal variation of soil respiration in the warming plots was closely coupled with that in the control plots, and both exhibited single-peak curves. The daily soil respiration in the warming was higher than that in the control from November 2014 to January 2015. Contrarily, from March to April 2015. During the non-growing seasons, there were no significant differences in the daily mean soil respiration between the two treatments. However, soil temperature and soil salt content in the warming plots were significantly higher than those in the control plots. The non-growing season was divided into the no salt restriction period (November 2014 to middle February 2015) and salt restriction period (middle February 2015 to April 2015). During non-growing season, soil respiration in the warming had no significant difference compared with that in control. During the no salt restriction period, soil respiration in the warming was 22.9% (p < 0.01) greater than the control when soil temperature at 10 cm depth in warming was elevated by 4.0 °C compared with that in control. However, experimental warming decreased temperature sensitivity of soil respiration (Q₁₀). During salt restriction period, soil warming decreased soil respiration by 20.7% compared with the control although with higher temperature (3.3 °C), which may be attributed to the increased soil salt content (Soil electric conductivity increased from 4.4 ds·m^-1 to 5.3 ds·m^-1). The high water content can limit soil respiration in some extent. In addition, the Q₁₀ value in the warming had no significant difference compared with that in control during this period. Therefore, soil warming can not only increase soil respiration by elevating soil temperature, but also decrease soil respiration by increasing soil salt content due to evaporation, which consequently regulating the soil carbon balance of coastal wetlands.     

棉花短季直播栽培模式对其农艺性状及干物质积累分配的影响

为探索棉花短季直播高产栽培模式,采用多因子最优混合设计(311设计)研究了播期、栽培密度和施氮量对早熟品种JX0010的农艺性状、干物质积累分配的影响。结果表明,不同处理对棉花生育进程有一定影响,播种期是影响棉花生育期的主要因子,各处理生育进程随播种期的推迟而缩短。不同处理株高、果枝层数、果枝始节、果节数差异都达到了显著水平,栽培因子对株高、果枝始节高度、果节数的影响大小顺序为密度施氮量播期,对果枝层数影响的顺序为播期密度施氮量,适量的施氮、合理密植以及适当推迟播期能增大植株高度,增加棉株果节数。不同处理棉花地上部分单株干物质积累、群体干物质积累、单株营养器官干物质积累、生殖器官干物质积累变化趋势基本呈"S"型,不同处理干物质分配系数表现出随着生育进程的推进,营养器官所占比重降低,生殖器官所占比重逐渐升高的趋势。     

凤眼莲超氧物歧化酶活性与抗寒性的关系

低温使凤眼莲叶内SOD活性降低,同时叶组织电解质外渗增加和TTG的还原力降低。用适量的联吡啶季胺盐(Paraquat)处理凤眼莲叶片,使超氧物歧化酶活性增强,则能减轻低温引起的伤害。试验提供了超氧物歧化酶与抗寒性有关的直接证据.     

海南岛尖峰岭地区热带植被生态系列的研究

 本文通过对海南岛尖峰岭地区热带植被随环境条件递变而变化的分析,反映出在一较短的水平距离内植被变化的多样性,并通过群落生态学方法的分析,说明尖峰岭地区的植被在种类组成、多样性、群落外貌等方面都具有较典型的热带性质,但在群落的结构方面则比典型的热带雨林逊色,说明它是地处热带北缘和在季风气候影响下的必然结果。用重要值方法来描述热带植物群落,其结果较为理想。研究该地区热带植被的特点,对认识、了解我国的热带植被和经营热带林等方面,提供了一些理论依据。     

河南雨林教育工程有限公司

河南雨林教育工程有限公司始建于1958年（原河南师范大学生物制片厂），我公司从建厂至今，已经走过了近49个年头。在近半个世纪的漫长岁月里，始终坚持了质量第一，服务教学的企业信仰，从只有一个小小的生物切片实验室发展成为现有3080余个品种系列,     

喀斯特季节性雨林优势树种叶片微形态与光合生理特征及其生态适应性

为深入理解喀斯特季节性雨林优势树种对异质性生境条件的适应策略，该研究以广西弄岗原生性森林7个优势树种为对象，测定各树种成年个体叶片微形态结构及生长季光合生理特征等指标，探讨树种叶片结构功能对喀斯特峰丛山地异质性生境的响应规律。结果表明：(1)沿喀斯特地貌部位的洼地-中坡-山顶生境梯度，树木的叶片紧密度、栅栏组织厚度、角质层厚度、上表皮厚度等9个微形态指标均呈显著上升趋势，叶片疏松度呈显著下降趋势。(2)沿洼地-中坡-山顶生境梯度，树木的光补偿点、暗呼吸速率、最大蒸腾速率等均呈显著上升趋势，最大水分利用效率、最大胞间CO₂浓度、表观量子效率等均呈显著下降趋势。(3)叶片紧密度与光合能力、蒸腾能力等相关指标则表现为显著正相关，叶片疏松度与这两类指标则表现为显著负相关。综上认为，喀斯特季节性雨林优势树种叶片功能性状存在光合效率和耐旱性之间的权衡，洼地生长的树木具有显著的弱光适应特征，中坡生长的树木表现较广的生境适应范围，山顶分布的树种因受强光、高温和裸岩限制而表现出较强的干旱适应特征以及保守的生态适应策略。     

生长季川陕不同地带植被覆盖对气候变化的时空响应

川陕地区处于中国800mm等降水量线过渡带的南北两侧,区内分山、川、原3种地形,是退耕还林(草)最早实施区域。基于2001—2014年的MODIS、气温和降水量数据,选取10种植被地带数据,采用Sen+MK检验和时滞偏相关等方法,结合重分类后的4种地貌类型和6类土地利用/覆盖数据,分年内生长季、年际生长季和非生长季的对比、以及植被生长最好的8月与5月、6月、7月、8月、5—6月、6—7月、7—8月、5—8月共8个时间段的相关性3种时间尺度,对川陕地区植被NDVI与气候因子的关系进行了深入探讨。结果表明:1)川陕、陕西和四川年均气温分别以0.02℃/10a、0.01℃/10a和0.03℃/10a(通过0.01显著性水平)的线性速度增加,低于近50年来(1951—2001年)全国的气温增速(0.22℃/10a);2)川陕、陕西、四川尺度上,植被NDVI与同季气温、降水量的相关性一致,与上季的相关性不具一致性。植被NDVI与上季气温、降水量的相关性均高于同季,相较于降水量,与气温呈现出更多的负相关性,其中陕西地区最为显著;3)川陕地区气温变化趋势与全球变暖不同步,植被生长受气温的影响较小或无影响;降水量相较于气温对陕西地区植被生长的影响更大;气温是四川植被生长的主要限制因素。植被覆盖与气温、降水量的相关性在草地、林地和农耕区最为显著。     

永定河沿河沙地杨树人工林生态系统呼吸特征

杨树是世界上广泛采用的人工造林树种之一,也是中国人工林面积最大的树种。研究杨树人工林生态系统呼吸(Re)及其分量土壤呼吸(Rs)的时间动态格局以及强度特征,分析两者对环境因子的响应是提高人工林生态系统净生产力和促进固碳减排等人工林经营管理中考虑的首要问题。采用开路式涡度相关系统、Licor-8150土壤呼吸测定系统以及小气候测定系统连续测定了位于北京大兴区永定河沿河沙地杨树人工林的生态系统呼吸、土壤呼吸和小气候特征。研究结果表明:(1)2007-2009年该生态系统的Re年总量分别为946.68、863.58、817.30gCm^-2a^-1,其中Rs年总量分别为642.11、629.29,609.05gCm^-2a^-1, Rs年总量约占Re年总量的70%;(2)Re和Rs月总量一般在7或者8月份达到最大值,Rs的变化趋势与土壤5cm温度(Ts5)相一致;(3)Ts5是Re和Rs两者的显著影响因子,但Re与空气相对湿度(RH)的相关性最显著。此外,Rs更容易受到Ts5和0-20cm土壤平均体积含水量(vwc)两者耦合效应的限制。     

西双版纳热带季节雨林粗木质物残体储量及其空间分布

粗木质物残体(CWD)在森林生态系统的物质循环和碳动态中发挥着重要作用,但目前国内对热带地区CWD储量与其空间分布关系上的研究还处于起步阶段。对西双版纳1hm2热带季节雨林样地调查发现,≥10cm的粗木质物残体占森林总凋落物量的68.02%,其中45.72%的CWD处于腐解中后期。由于多数大径级的CWD分布于15°～25°的坡地上,且其饱和持水力随腐解等级的增加而上升,因此,CWD将有助于改善坡地生境下的水肥条件。CWD的分布受风向和本地湿热环境的影响,但掉落指向则更倾向于随机过程。CWD产生和分布上的普遍性有可能对森林生境异质性和生物多样性产生重大影响。     

N,N,N-三甲基壳聚糖甲基硫酸盐的合成及理化性质的测定

壳聚糖与甲醛、甲酸反应得到N,N-二甲基壳聚糖,然后以硫酸二甲酯为季铵化试剂反应得到N,N,N-三甲基壳聚糖甲基硫酸盐(TMCMS),用IR1、H NMR和元素分析对其结构进行了表征。元素分析结果表明其季铵化度为74.6%,差示扫描量热法和热重分析法结果表明其热稳定性比壳聚糖差,但其水溶性明显优于壳聚糖,25℃时在水中的溶解度可达20 mg/mL,浓度为2 mg/mL时在pH 3～12范围内无沉淀产生。