基于APSIM模型的不同施肥处理下春玉米产量模拟及气候敏感性分析

以平凉市泾川县大田试验为基础,利用农业生产系统模拟模型,探究不同类型施肥处理对春玉米产量的影响以及气候变化对春玉米产量影响的敏感性差异,分析APSIM模型对模拟该地区春玉米产量的适应性。结果表明,APSIM模型对该区域春玉米产量的模拟效果较好,决定系数(R²)介于0.934～0.975,归一化均方根误差(NRMSE)介于6.073%～9.758%,模型一致性指标(D)介于0.952～0.987。模型敏感分析显示,年平均温度是模拟不同施肥处理下春玉米产量的敏感参数,其变化程度对模拟结果影响较大,不同施肥处理(CK、N、NP)下的敏感指数分别为0.533 2、0.558 7和0.568 2。     

陕北黄土区退耕还林(草)地土壤质量特征及其对降水的响应

为了解陕北黄土区退耕还林（草）地土壤质量差异特征及其对降水的响应,该文沿370～470 mm的降水梯度,选取了陕西省吴起县境内的王洼子（370～395 mm）、大吉沟（440～445 mm）和白豹（460～470 mm）3个降水梯度区作为研究区,并结合土壤质量指数法,定量评价降水梯度区广泛栽植的刺槐林（Robinia pseudoacacia）、沙棘林（Hippophae rhamnoides）和草地的土壤物理结构、持水性、盐碱度、碳汇指标以及速效养分指标方面的综合得分,明确植被恢复后土壤质量随降水梯度的变化特征。结果表明：1）降水量、植被类型以及二者的交互作用对土壤指标影响显著（P<0.05）。2）在460～470 mm降水量区,刺槐林（0.829）对土壤质量改良效果最好,其次为沙棘林（0.808）,二者土壤质量均达到肥沃水平,且差异不显著,草地（0.679）土壤质量指数最低,土壤为较肥沃水平;在440～445 mm降水量区,沙棘林（0.74）对土壤改良效果最好,其次为刺槐林（0.601）,二者均达到较肥沃水平,草地（0.479）土壤质量指数最低为中等水平;在370～395 mm降水量区,3种植被类型土壤质量指数由大到小表现为沙棘林（0.744）>刺槐林（0.387）>草地（0.251）,沙棘林土壤质量等级为较肥沃、刺槐林和草地为贫瘠水平。3）在370～470 mm降水梯度内,3种植被类型土壤质量综合指数均随着降水量的减少而降低,其中沙棘林土壤质量指数变异性较低（4.1%）,刺槐林（30.1%）和草地（37.2%）土壤质量变异性较高。该研究结果可为陕北黄土区370～470 mm降水梯度下的植被恢复与重建等林业生态工程实施提供数据支撑与理论支持。     

呼伦贝尔市2011年大豆生长季气候影响分析

2011年呼伦贝尔市大豆种植62.62万hm2,比2010年增加4.68万hm2。通过2011年气候资料的统计分析,得知在大豆生长季气温稍低,降水正常或局部偏多,大部分地区光照偏少,光、水、热匹配较好,尤其是水分条件对需水较多的大豆生长较为有利。     

基于灰色关联原理分析北亚热带次生竹林降雨分配影响因素

为了解北亚热带次生毛竹林降雨分配功能与各影响因素之间的关系，运用灰色关联分析方法计算了影响林分降雨分配各因素的灰关联度值．揭示了降雨分配过程中的主导影响因素。     

甘肃省干旱半干旱地区降水的研究

本文通过对甘肃省降水资料的具体分析,指出了在干旱、半干旱地区降水的主要特征,如暴雨的特殊性、固体降水与海拔关系、降水量与海拔关系、降水量与作物产量关系等,并对如何提高降水利用率,发展农业生产等问题进行了探讨。     

新疆山区降水资源及其开发利用

本文论述了新疆山区的降水特征及其空间与时间上的分布规律,提出了合理利用降水资源的意见。     

Changes in anthropogenic impervious surfaces,precipitation and daily streamflow discharge: a historical perspective in a mid-atlantic subwatershed

Aerial photography provides a historical vehicle for determining long-term urban landscape change and, with concurrent daily streamflow and precipitation records, allows the historical relationship of anthropogenic impervious surfaces and streamflow to be explored. Anthropogenic impervious surface area in the upper Accotink Creek subwatershed (near Annandala, Virginia, USA) was mapped from six dates of rectified historical aerial photography ranging from 1949 to 1994. Results show that anthropogenic impervious surface area has grown from approximately 3% in 1949 to 33% in 1994. Coincident to this period, analysis of historical mean daily streamflow shows a statistically significant increase in the streamflow discharge response (per meter of precipitation) associated with normal and extreme daily precipitation levels. Significant changes were also observed in the frequency of daily streamflow discharge at given volumes above and below the historical daily mean. Simultaneously, the historical magnitude, frequency and pattern of precipitation values 0 mm, 6.0 mm and 35.0 mm show either no statistically significant change or influence on streamflow. Historical changes in streamflow in this basin appear to be related to increases in anthropogenic impervious surface cover. Historical aerial photography is a viable tool for revealing long-term landscape and ecosystem relationships, and allows landscape investigations to extend beyond the temporal and spatial constraints of historical satellite remote sensing data.This revised version was published online in May 2005 with corrections to the Cover Date.     

Simulated rain addition modifies diurnal patterns and temperature sensitivities of autotrophic and heterotrophic soil respiration in an arid desert ecosystem

The timing and magnitude of rainfall events in arid and semiarid regions are expected to change dramatically in future decades, which will likely greatly affect regional carbon cycles. To understand how increases in rainfall affect the diurnal patterns and temperature sensitivities (Q₁₀) of soil respiration (R_S) and its key components (i.e. heterotrophic respiration (R_H) and autotrophic respiration (R_A)), we conducted a manipulative field experiment in a desert ecosystem of Northwest China. We simulated five different scenarios of future rain regimes (0%, 25%, 50%, 75% and 100% increase over local annual mean precipitation) each month from May to September in 2009. We measured R_S and R_H every three hours on 6 and 16 days after the rain addition, and estimated R_A by calculating the difference between R_S and R_H. We found that rain addition significantly increased the daily mean R_S and its components on the two measurement days during the growing season. However, the diurnal pattern was different between the two respiration components. Rain addition significantly increased the daily Q₁₀ value of R_H but suppressed that of R_A on Day 6. Rain addition had no influence on daily Q₁₀ value of both respiration components on Day 16 when soil moisture was lower. In addition, we observed significantly higher daily Q₁₀ of R_H than R_A under all five rain addition treatments, indicating that microbial respiration is more temperature sensitive than root respiration in a short-time scale in this desert ecosystem. Thus, partitioning soil respiration into its two components, and analyzing the differential responses of R_H and R_A to future climate changes should be considered for more accurate predictions of soil respiration and regional carbon cycle in these arid and semiarid regions.     

竹林养分循环规律研究：Ⅲ.毛竹纯林竹秆流及其养分输入

在我国毛竹主要产区浙江省安吉县灵峰寺林场试验林的三个区组中，根据立竹直径分布规律确定样竹处理数后，随机布置总共30套秆流收集装置，持续观察21个月，共获91次秆流水。测定每次秆流水量并分析其N、P、K、Ca、Mg含量以研究毛竹林内秆流的变化动态及其养分输入。结果表明：秆流水中不含Ca，其它四元素的年输入量分别为N-1．8557，P-0．0072，K-0.7849，Mg-0.1569，Kg.ha－1；年秆流量为年降水量的12．5％，无论次、月秆流量与相应降水量均为紧密线性相关，但与立竹粗度为显著非线性相关；其它因子，如：立竹所处的坡位、坡向，竹林密度，钩梢强度，立竹分布状况，植株个体表面结构特征等，亦直接或间接地影响着竹秆流的产生和大小。     

民勤沙区降水及干旱特征分析

民勤干旱沙区降水稀少，３４年年平均降水量为１１３．２ｍｍ，且季节分布不均，年际变化大，平均降水变率为２４．５％，降水年变化规律呈正态分布。降水性质多以日降水量≤１０．０ｍｍ的小雨为主。持续干旱日数长，发生频率高，属典型干旱荒漠气候。