地埋滴灌点源入渗土壤水分运动规律实验研究

通过室内砂土中进行地埋滴灌的实验,对地埋滴灌在砂土中的适应性进行初步研究,为田间试验布置提供依据。通过分析湿润锋的推移速率、特征点的土壤含水率变化规律,发现湿润锋推移速率先是径向大于垂向,随着灌水时间和灌水量增加,水平方向和垂向的湿润锋和含水率趋于平衡。根据对比滴灌带埋深15和20 cm特征点的含水率变化情况,得出埋深15 cm节水效果更好,更利于作物生长。实验还得出湿润比能作为滴灌灌水参数的指标,由于作物种植的间距和作物根系深度之比基本小于1.0,因此在田间实际灌溉中湿润比应控制在1.0左右。     

施氮深度对‘黄金梨’树氮素吸收、分配及利用效率的影响

以7年生‘黄金梨’树为试材,采用~(15)N示踪技术研究了3个施氮深度[0(表面施氮)、20和40 cm]处理下不同器官对氮素的吸收、分配及利用效率,并探讨了氮素在土壤中的残留及损失。结果表明,梨果实成熟期,果实的Ndff值最高,其他器官的Ndff值均表现为20 cm施氮深度处理显著高于其他处理。各施氮深度处理,~(15)N的分配率均为贮藏器官最高,生殖器官最低。20 cm施氮深度处理的梨树N利用率最高(26.23%),40 cm施氮深度处理最低(15.65%)。N损失率以表面施氮处理最高(54.21%),20 cm施氮深度最低;0~80 cm土层的N残留率以40 cm施氮深度处理最高(31.73%),表面施氮处理最低。因此,本研究中,20 cm深度施氮处理能提高梨树各器官对N肥的吸收征调能力,氮素损失少。     

Simulating farming practices within a region using a stochastic bio-decisional model: Application to irrigated maize in south-western France

Agricultural is a major contributor to environmental resource management problems. Modelling the distribution of agricultural land use to evaluate current situations or scenarios is an important issue for policy-makers and natural resource managers. A promising approach is the use of bio-decisional models based on decision rules. However, at the regional scale, the large number of farmers makes it difficult to identify decision rules, and the diversity of farmers' decisions is rarely considered. To this end, we developed SIMITKO, a spatialised and stochastic bio-decisional model, able to simulate the spatial and temporal variability in farming practices. We focused on the choice of varietal earliness and sowing practices of maize (Zea mays L.) in the Baïse sector (south-western France). Model development was based on statistical analyses of surveys of farmers’ practices to identify their current strategies, the best variables to describe the practices and the probabilities associated with the values of the variables for each strategy. We tested SIMITKO by simulating the dynamics of areas sown with maize. Comparing model predictions of practices to observed data showed generally good predictions of sowing dynamics but less satisfactory predictions of varietal earliness choices. Possible improvements are suggested.     

梯形明渠水力学特征水深的解析计算式研究

通过数学理论分析,推出了梯形明渠的临界水深和正常水深高精度解析计算式,并与现有文献相关计算式进行了对比分析。结果表明,新推出的临界水深计算式相对误差小于0.3%;当梯形明渠坡比0.1~7时,新推出的正常水深初值计解析算公式相对误差一般小于3%;另外,给出了收敛速度更快的正常水深迭计算公式,且在m1时正常水深计算公式在初值迭代一次后其误差均小于0.5%。新推出的梯形明渠临界水深和正常水深解析计算式方便简捷、精度可靠。     

Impact of winter‐to‐spring environmental variability along the Kuroshio jet on the recruitment of Japanese sardine (Sardinops melanostictus)

Winter‐to‐spring variability in sea surface temperature (SST) and mixed layer depth (MLD) around the Kuroshio current system and its relationship to the survival rate (ln [recruit per spawning stock biomass], LNRPS) of Japanese sardine (Sardinops melanostictus) were investigated based on a correlation analysis of data from 1980 to 1995. The data were from a high‐resolution ocean general circulation model using the ‘Kuroshio axis coordinates’, in which the meridional positions are relocated to a latitude relative to the Kuroshio axis at each longitude, rather than the geographically fixed coordinates. A significant positive (negative) correlation between LNRPS and winter MLD (winter–spring SST) was detected near the Kuroshio axis from areas south of Japan (where eggs are spawned) to the Kuroshio Extension (where larvae are transported). This result is in contrast to previous studies using geographically fixed coordinates, which showed a significant correlation predominantly in the area south of the Kuroshio Extension in winter, where at this time few larvae have been found. From the late 1980s to early 1990s, when the survival rate was remarkably low, MLD around the axis was shallow and SST was high. Although MLD and SST show a significant correlation, significant partial correlations were also observed between February MLD and LNRPS when the contribution of SST was excluded, and between March SST and LNRPS when the contribution of MLD was excluded. We presume that MLD shoaling reduced the nutrient supply from deep layers, resulting in less productivity in the spring, and SST warming could have a negative influence on larval growth.     

金枪鱼围网沉降特性

根据沿围网下纲缚扎的10只温度深度计(TDR-2050型)自动记录的23网次有效数据,对中国中西太平洋金枪鱼围网的下纲沉降速度、沉降深度及其与时间的关系进行了研究。结果表明:(1)网具未达到理论沉降深度,网具中部平均沉降深度为160 m,为最大拉紧高度(311.1 m)的51.4%;(2)网具中部沉降深度与时间的关系为h=–0.000 2t2+0.3663 t;(3)网具各部位的沉降速度不同,取鱼部最慢,网具中部次之,后网头最快;(4)下纲各部位沉降速度均随着深度的增加而减小,沉降速度波动幅度随深度增加按大—小—大的规则变化;(5)网具中部沉降速度与时间的关系为:v=3×10–7t2–7×10–4 t+0.418 9。本研究结果可为改善金枪鱼围网沉降性能提供基础数据,并为海上生产提供指导性参考。     

兴仁小白壳薏苡不同播期对产量的影响

为探索适宜兴仁县薏苡种植的最佳播种时期，在兴仁县开展了薏苡不同播期对产量影响的试验。试验共设9个播期，梯度为7 d，播种时间从3月19日－5月14日。试验结果表明，兴仁小白壳薏苡的最佳播期是3月19日－4月16日，并且在此期间播种，薏苡产量较高。     

氧化塘深度对猪场厌氧消化液后处理的影响

采用小试装置对3个不同深度氧化塘处理猪场厌氧消化液的效果进行了研究,结果表明:当平均气温为21.9℃,停留时间在80 ～110天,进水负荷为0.05 m3·m-2d-1的条件下,氧化塘对NH4-N的去除率达到了90％以上,CODcr,TP的去除率分别为50％,40％.硝化作用和藻类的吸收是氧化塘去除NH4-N的主要方式,沉淀作用则是CODcr和TP的主要去除方式,在较长停留时间下,微生物对于溶解性CODcr的分解和同化也能提供一定的去除效果.当平均气温为21.9℃,在表面负荷为0.05 m3·m-2d-1的条件下,有效深度为0.3m和0.7m的氧化塘面积去除负荷分别为1.41 g·m-2d-1,1.49 g·m-2d-1,容积去除负荷分别为4.7g·m -3d-1,2.8g·m-3d-1.虽然较深氧化塘具有较高的面积去除负荷,但较浅的氧化塘却有更高的容积去除负荷.     

排灌输水隧洞正常水深的简捷算法

为了使标准城门洞形断面正常水深的求解具有简单的显函数计算公式,对标准城门洞形断面正常水深的基本方程进行恒等变形,将水面位于底角圆弧段和顶弧段正常水深的超越方程以及水面位于侧边直线段正常水深的高次方程,变成无量纲化正常水深与已知量综合参数的单变量函数方程.引入准线性函数的概念并将准线性函数作为标准模板,再对正常水深的单变量函数方程应用准线性函数标准模板,在工程常用范围即无量纲化正常水深y∈[0.051,.80]范围内进行优化计算及准线性函数逼近,得到了超越方程和高次方程的替代函数方程,替代函数具有类似于线性函数形式,即正常水深的准线性显函数表达式,并进行误差分析.结果表明,在隧洞底部圆弧段正常水深的最大相对误差小于0.36%,侧边直线段正常水深的最大相对误差小于0.31%,顶弧段正常水深的最大相对误差小于0.39%,说明准线性公式在隧洞有效水深范围内计算的水深准确度较高,可为排灌输水隧洞的断面设计及实现渠道水位控制时确定均匀流水深提供参考.     

基于水盐生产函数的绿洲灌区水盐调控研究

土壤次生盐碱化是新疆灌溉农业所面临的最大环境问题。灌溉农业的快速扩展与灌排系统不完善是造成土壤次生盐碱化发生与恶化的关键因素。以水盐生产函数为依据,计算了不同生育阶段及全生育期阶段棉花相对产量与土壤全盐的关系,依据该计算结果对塔里木灌区的土壤盐化程度做了初步划分。基于塔里木灌区地下水埋深较浅且多为微咸水的事实,比较深入地探讨了地下水合理的动态水位及作物对潜水利用问题。最后,提出了灌区水盐调控的对策,强调排水系统的通畅运行是控制土壤次生盐碱化的关键,通过排水系统和减少灌溉定额使作物生长期的地下水埋深控制在1.6~2.1 m内,不但可以减少排水成本,而且也可使作物充分利用地下水,同时促进塔里木河水质的改善。