Knowledge Resource Center for Ecological Environment in Arid Area
陕西黄土高原中南部土壤CO_2释放量变化研究 | |
其他题名 | A Study on the Flux of CO_2 Release in the Middle and South of the Plateau in Shaanxi |
贺辉; 赵景波; 杜娟; 童心刚; 郝玉芬; 刘晓琼 | |
来源期刊 | 干旱区资源与环境
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ISSN | 1003-7578 |
出版年 | 2003 |
卷号 | 17期号:5页码:49-53 |
中文摘要 | 本文根据NaOH溶液吸收CO_2的方法,对陕西黄土高原中南部4个观测点的土壤CO_2释放量时行了昼夜观测。观测结果表明,不同地区、不同气候和不同土质土壤CO_2释放量存在差异,冷干地区较暖湿地区土壤CO_2释放量少,凉季较暖季土壤CO_2释放量少;粘性硬质土较松散黄土CO_2释放量少。长武、洛川、西安南郊土壤CO_2释放量变化再次证明,在厚层黄土发育的地区,土壤CO_2翻译量变化相对于大气温度变化具有滞后性,从当日早晨至次日早期,CO_2翻译量具有由低变高再变低的普遍规律。 |
英文摘要 | By means of CO_2 absorption by NaOH solution, the flux of CO_2 release in four research areas was observed in the middle south of Loess Plateau in Shaanxi. Results show that there are differences a-mang flux of CO_2 released in different areas, different climate and different geological conditions. The release flux is lower in cool and arid area than that in warm and moist area, and it is lower in cool season than that in warm season; and it is also lower in hard soil than that in loose soil. The flux of CO_2 release in Chanwu, Luochuan and the south of Xi’an area proved again that the flux of CO_2 release from soil is about 4-6 hours later than that of air temperature change, and the release flux changes from low to high and then to low from this morning to the next, which is general regularity of the change of release flux of CO_2 on thick loess layer. |
中文关键词 | 黄土高原中部 ; 土壤CO_2 ; 释放变化 ; 影响因素 |
英文关键词 | the middle and south of the loess plateau CO_2 of soil the change of release flux effecting factors |
语种 | 中文 |
国家 | 中国 |
收录类别 | CSCD |
WOS类目 | AGRICULTURE MULTIDISCIPLINARY |
WOS研究方向 | Agriculture |
CSCD记录号 | CSCD:1199183 |
来源机构 | 陕西师范大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/204103 |
作者单位 | 陕西师范大学地理系, 西安, 陕西 710062, 中国 |
推荐引用方式 GB/T 7714 | 贺辉,赵景波,杜娟,等. 陕西黄土高原中南部土壤CO_2释放量变化研究[J]. 陕西师范大学,2003,17(5):49-53. |
APA | 贺辉,赵景波,杜娟,童心刚,郝玉芬,&刘晓琼.(2003).陕西黄土高原中南部土壤CO_2释放量变化研究.干旱区资源与环境,17(5),49-53. |
MLA | 贺辉,et al."陕西黄土高原中南部土壤CO_2释放量变化研究".干旱区资源与环境 17.5(2003):49-53. |
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