期刊文献+
共找到4篇文章
< 1 >
每页显示 20 50 100
西安地区S_4古土壤剖面中古水分指标与水环境研究 被引量:1
1
作者 赵景波 马延东 +2 位作者 罗小庆 邵天杰 刘瑞 《地质学报》 EI CAS CSCD 北大核心 2017年第3期678-689,共12页
通过野外调查和实验分析,在西安蓝田安村黄土剖面S_4古土壤剖面中发现了具有指示当时土壤水分含量、地下水富集和水分循环的铁锰结核、针铁矿[α-FeO(OH)],在西安地区确定了风化淋滤黄土层和显著迁出了土壤黏化层的CaCO_3结核淀积层。... 通过野外调查和实验分析,在西安蓝田安村黄土剖面S_4古土壤剖面中发现了具有指示当时土壤水分含量、地下水富集和水分循环的铁锰结核、针铁矿[α-FeO(OH)],在西安地区确定了风化淋滤黄土层和显著迁出了土壤黏化层的CaCO_3结核淀积层。针铁矿呈褐黄色薄膜分布于土体表面,含量可达3.3%。铁锰结核呈黑褐色球形,电镜下多呈结晶粒状,铁锰成分含量很高。针铁矿和铁锰结核富集层厚0.6m,形成于紧靠地下水的位置。通过研究提出了铁锰结核和风化淋滤黄土层及CaCO_3结核淀积层可作为恢复土壤古水分含量的重要指标。针铁矿、铁锰结核和风化淋滤黄土层的形成以及CaCO_3结核与红色铁质胶膜的迁移深度指示,在S_4古土壤发育时期,西安地区为亚热带气候,当时年平均气温为15~16℃,年平均降水量在900~1000mm之间。那时秦岭失去了亚热带与温带气候分界线的作用。在S_4古土壤发育时期,西安地区土壤重力水分布深度达到了3.3m,当时土壤水在经过蒸发与蒸腾消耗之后,3.3m深度范围内剩余的土壤平均含水量一般为25%左右,在针铁矿和与铁锰结核发育层位含水量接近饱和(50%左右)。当时土壤水分非常充足,水分循环正常,水分平衡为正,有较多水分补给地下水,适于茂盛森林植被发育。本文所确定的古含水量指标为国内外第四纪土壤含水量、水分存在形式与水循环研究提供了标准和方法。 展开更多
关键词 S4古土壤 铁锰结核与针铁矿 古水循环 含水量指标 水分平衡 西安地区
下载PDF
Research Progress of Evaluation Index of Soil Moisture 被引量:2
2
作者 林坡 马友华 +4 位作者 江朝晖 王强 王静 黄浩 江宏 《Agricultural Science & Technology》 CAS 2016年第4期968-971,988,共5页
In modern agriculture, accurate and effective measurements of soil water content lays foundation for promotion on precision irrigation technology and improvement on water use efficiency. The research reviewed soil moi... In modern agriculture, accurate and effective measurements of soil water content lays foundation for promotion on precision irrigation technology and improvement on water use efficiency. The research reviewed soil moisture indices at home and abroad and classified the indices into two categories in order to make prediction on soil moisture and take measures. Specifically, single indices included precipitation index, soil moisture index, and crop drought index and overall indices included supply/demand water index of crops, overall water index, PDSI, crop water shortage index. Soil moisture index was analyzed in terms of advantages and disadvantages,as well as adaptability in agriculture, providing references for relieving and predicting adverse effects on agriculture and formulating scientific policies. 展开更多
关键词 Soil moisture index Soil moisture PROCESS EVALUATION
下载PDF
Effects of Water Stress on Leaf Water and Chlorophyll Fluorescence Parameters of Sugarcane Seedling 被引量:11
3
作者 朱理环 邢永秀 +4 位作者 杨丽涛 李杨瑞 杨荣仲 莫磊兴 Li-huan Yong-xiu Li-tao Yang-rui Rong-zhong Lei-xing 《Agricultural Science & Technology》 CAS 2010年第5期17-21,共5页
[Objective] The aim was to explore the effects of water stress on leaf water and chlorophyll fluorescence parameters of sugarcane seedling,as well as to provide basis for the study on sugarcane production and evaluati... [Objective] The aim was to explore the effects of water stress on leaf water and chlorophyll fluorescence parameters of sugarcane seedling,as well as to provide basis for the study on sugarcane production and evaluation. [Method] Seven different sugarcane varieties were studied at the seedling stage under drought stress,and the changes of leaf water and chlorophyll fluorescence parameters under stress conditions were detected. [Result] leaf water potential,leaf relative water content and soil relative water content showed a certain amount of internal relationship,the sugarcane varieties that had more tolerant to drought had higher utilization rate of soil water; the correlation analysis and factor analysis suggested that the survival rate at seedling stage under drought stress,Fv/Fm,leaf water potential and relative water content could be used as drought resistance evaluation indicators. [Conclusion] As a relatively independent influencing factor,water potential had dominating effect on drought resistance,and the reliability of Fv/Fm as drought resistance evaluation indicator had been verified. 展开更多
关键词 Sugarcane Drought stress Leaf water Leaf relative water content Fv/Fm
下载PDF
Degradation of Wetlands on the Qinghai-Tibet Plateau:A Comparison of the Effectiveness of Three Indicators 被引量:16
4
作者 GAO Jay LI Xi-lai +1 位作者 CHEUNG Alan YANG Yuan-wu 《Journal of Mountain Science》 SCIE CSCD 2013年第4期658-667,共10页
The Qinghai-Tibet Plateau encompasses a large quantity of wetlands, some of which have been degraded to varying severity levels. In the literature, a number of degradation indicators have been proposed to evaluate eco... The Qinghai-Tibet Plateau encompasses a large quantity of wetlands, some of which have been degraded to varying severity levels. In the literature, a number of degradation indicators have been proposed to evaluate ecological health of wetlands, but their effectiveness in the plateau environment remains unknown. In this study, we assessed the effectiveness of three degradation indicators, soil moisture content at lo em deep, vegetative cover, and density of pika burrows. The degradation severity of wetlands in Maduo County on the Qinghai-Tibet Plateau is enumerated at four levels, intact, slight, moderate and severe. Analysis of xo6 samples collected in the field demonstrates that the density of pika burrows is the least reliable indicator. By comparison, vegetative cover and underlying soil moisture content are more reliable, even though neither is a perfect indicator as the difference among adjacent levels of severity as revealed by t-test is not always statistically significant. The imperfection of vegetative cover as an indicator is due to its variation among different types of wetlands. The limitation of moisture content is attributed to its non-linear relationship with wetland degradation. Above the threshold of about 50% in moisture content wetlands are unlikely to be degraded. It is recommended that moisture be measured at the point near the surface and vegetative cover be further differentiated by species in order to improve their effectiveness. 展开更多
关键词 Wetland degradation Grass cover Soilmoisture Pika damage Qinghai-Tibet Plateau
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部