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991.
Soit carbon (C) stock is the largest C pool in terrestrial ecosystems, and the emission of CO2 through soil respiration contributes to the majority of soil C expenditure and atmospheric C. Soil respiration is also one of the major processes controlling the C budget of terrestrial ecosystems. A slight change in soil CO2 emission might cause drastic variations in global C balance. Therefore, it is of great significance to investigate the characteristics of soil respiration of soils growing different types of vegetation over a long period, and determine its relationship with variables such as soil temperature and moisture. The rate of soil respiration was measured each month in the growing seasons (from April to October) of 2011, 2013, and 2014 using the Li-8100 CO2 flux measurement system in the central Loess Plateau. Four types of vegetation (Quercus liaotungensis, Platycladus orientalis, Robinia pseudoacacia, and a natural shrub) were chosen for the periodical measurements. A permanent sample plot was established for each type of vegetation, and five polyvinyl chloride (PVC) collars were placed in each plot for the measurements. The temperature and water content of the soil in the upper 12 cm near the collar were measured using a digital soil temperature probe and a TDR 200 soil moisture meter at the same time when the soil respiration was measured. The soil respiration rates were fitted to the soil temperature and moisture with an exponential function, power function, linear function, and an equation combining the two variables. The results showed that: (1) the seasonal variation in the rates of soil respiration in the soils growing the four types of vegetation were almost the same, and were lower in the earlier period and then increased to high levels in the middle and later periods; (2) the rates of soil respiration in the same month varied with the type of vegetation grown, and were in the descending order: Q. liaotungensis > P. orientalis > shrub > R. pseudoacacia; (3) the average values of the rates of soil respiration in 2011, 2013, and 2014 were 2.77, 3.48, and 5.08 μmol m-2 s-1, respectively. The variation in soil respiration was higher across the three years than the variation for the types of vegetation grown; and (4) the rate of soil respiration was positively correlated to soil temperature and moisture for all the types of vegetation. A better fit was obtained by using the equation that included both the variables, soil temperature and moisture, than by an equation that included a single factor. Our results suggested that both seasonal and inter-annual variations of soil respiration occurred in the soils growing the four types of vegetation in the region. The temperature and water content of soils are the major regulating factors, and soil respiration in the Loess Plateau is more greatly affected by environment factors than by the type of vegetation. © 2018 Science Press. All rights reserved. 相似文献
992.
Shuo Wei Lei Du Shuo Chen Hongtao Yu Xie Quan 《Frontiers of Environmental Science & Engineering》2021,15(1):11
993.
Integrating Stressor and Response Monitoring into a Resource-Based Water-Quality Assessment Framework 总被引:1,自引:0,他引:1
Dirk J. Roux Phillip L. Kempster Cornelius J. Kleynhans Henk R. Van Vliet Hein H. Du Preez 《Environmental management》1999,23(1):15-30
Following a global trend, the new policy goals emphasize the need to protect rather than to use the ability of ecosystems
to recover from disturbances. This necessitates the adoption of response measurements to quantify ecological condition and
monitor ecological change. Response monitoring focuses on properties that are essential to the sustainability of the ecosystem.
These monitoring tools can be used to establish natural ranges of ecological change within ecosystems, as well as to quantify
conceptually acceptable and unacceptable ranges of change. Through a framework of biological criteria and biological impairment
standards, the results of response monitoring can become an integral part of future water resource management strategies in
South Africa. 相似文献
994.
995.
996.
南极菲尔德斯半岛植被土壤N2O排放特征 总被引:2,自引:0,他引:2
应用密闭箱法首次测定了南极菲尔德斯半岛苔藓、地衣植被土壤N2O的排放通量,并估算了该半岛植被区土壤在夏季2个月内N2O的排放总量.结果表明:在晴天和雨天,苔藓土壤N2O的排放通量与温度有较好的响应关系,呈现单峰型变化趋势;但在雪天,与温度的变化不一致;苔藓、地衣这2种不同的植被土壤N2O排放通量日变化基本一致;温度是影响苔藓土壤N2O的排放通量季节变化的主要因子,同时还受降水的影响,干湿交替有利于N2O的排放;苔藓土壤N2O的排放总量为3.7152kg;地衣土壤N2O的排放总量为2.5344kg.由此可见,南极菲尔德斯半岛苔藓、地衣植被土壤N2O排放量虽然很小,但仍起着大气N2O源的作用. 相似文献
997.
石油化工系统污泥处理研究 总被引:5,自引:2,他引:3
石油化工系统污水处理产生的污泥同城市污水处理产生的污泥有一定区别,针对兰州石化公司炼油化工污泥其固有的组分特点,并通过转筒离心机、板框压缩机、带式压滤机、真空过滤机等不同机械脱水方式的比较,提出了这类污泥在处理和处置时应注意的问题及几点建议。 相似文献
998.
When and how often to release information on television are important issues in crisis and emergency risk communication. There is a lot of crisis information, including warnings and news, to which people should have access, but most of it is not significantly urgent to interrupt the broadcasting of television programmes. Hence, the right timing for the release of crisis information should be selected based on the importance of the crisis and any associated communication requirements. Using recursive methods, this paper builds an audience coverage model of crisis information release. Based on 2007 Household Using TV (HUT) data for Hefei City, China, the optimal combination of broadcasting sequence (with frequencies between one and eight times) is obtained using the implicit enumeration method. The developed model is applicable to effective transmission of crisis information, with the aim of reducing interference with the normal television transmission process and decreasing the psychological effect on audiences. The same model can be employed for other purposes, such as news coverage and weather and road information. 相似文献
999.
1000.
以往对风电塔架研究大多采用刚性地基的假定,忽略土—结构的动力相互作用。然而风电塔架在实际地震时,由于地基的柔性和无限性,使得按刚性地基假定计算出来的结构动力特性和动力反应与将地基和结构作为一个整体计算出来的结果有较大差别。因此,考虑土—结构相互动力作用(SSI)的风电塔架地震响应分析研究十分必要。以华能阜新风力发电塔架为例,基于复模态法分析考虑土—结构相互作用风电塔架地震响应,首先建立土—风电塔架体系计算模型,采用Novak模型对伐板的复刚度、复阻尼计算,然后建立土—风电塔架相互作用体系的地震反应方程,采用复模态分析方法对结构地震反应求解,可供风电塔架抗震设计参考。 相似文献