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Parameterizing an agricultural production model for simulating nitrous oxide emissions in a wheat–maize system in the North China Plain 被引量:3
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作者 LI Ting-Ting ZHANG Wei +4 位作者 WANG Jun ZHANG Wen WANG Guo-Cheng XU Jing-Jing ZHANG Qing 《Atmospheric and Oceanic Science Letters》 CSCD 2016年第6期403-410,共8页
Concentrations of atmospheric nitrous oxide (N2O), a potent greenhouse gas, have been continuously increasing, and cropland soils are one of the largest sources of N2O. Variations in environmental and anthropogenic ... Concentrations of atmospheric nitrous oxide (N2O), a potent greenhouse gas, have been continuously increasing, and cropland soils are one of the largest sources of N2O. Variations in environmental and anthropogenic factors have substantial impacts on both the frequency and magnitude of N2O emissions. Based on measurements from a wheat-maize system in the North China Plain, the authors parameterized the Agricultural Production Systems Simulator (APSIM) model, which was initially developed in Australia, for simulating N2O emissions under different agricultural management practices. After calibrating one of the key parameters -- the fraction of N2O lost in nitrification (k2) -- the results showed that the model successfully captured the daily N2O fluxes under different nitrogen fertilization treatments, but underestimated some large peak fluxes. By pooling all data together, the calibrated APSIM model also performed well in representing cumulative N2O emissions under various treatments at annual and finer (monthly and daily) time scales. 展开更多
关键词 Agricultural productionmodeling nitrous oxide wheat-maize system North China Plain
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中朝板块新元古代微亮晶(臼齿构造)碳酸盐事件、层序地层和建系研究 被引量:8
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作者 孟祥化 葛铭 刘燕学 《地层学杂志》 CSCD 北大核心 2006年第3期211-222,共12页
通过对中朝板块燕山、吉辽和徐淮地区新元古代地层的沉积学、旋回地层学、锶同位素地层学以及(臼齿构造)碳酸盐岩事件和海平面变化研究,特别是IGCP447项目的全球性综合调查和对比研究,提出了增建北华系的地层划分和对比方案:以南华系底... 通过对中朝板块燕山、吉辽和徐淮地区新元古代地层的沉积学、旋回地层学、锶同位素地层学以及(臼齿构造)碳酸盐岩事件和海平面变化研究,特别是IGCP447项目的全球性综合调查和对比研究,提出了增建北华系的地层划分和对比方案:以南华系底界(730±10Ma)也就是全球性成冰系的底界为北华系的顶界,而北华系底界应该对应于青白口系顶界(850Ma),即以钓鱼台组底界作为青白口系与北华系的界线。辽宁大连金石滩剖面可以作为北华系界线层型剖面的候选剖面。 展开更多
关键词 中朝板块 新元古代 年代地层 层序地层 北华系
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Climatic change features of fog and haze in winter over North China and Huang-Huai Area 被引量:21
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作者 YIN ZhiCong WANG HuiJun GUO WenLi 《Science China Earth Sciences》 SCIE EI CAS CSCD 2015年第8期1370-1376,共7页
This paper revealed the climatic change characteristics of fog and haze of different levels over North China and Huang-Huai area(NCHH).It was found that the haze-prone period has changed from winter into a whole year,... This paper revealed the climatic change characteristics of fog and haze of different levels over North China and Huang-Huai area(NCHH).It was found that the haze-prone period has changed from winter into a whole year,and the haze days(HD)in winter have increased significantly.The foggy days(FD)are half of HD.There are little difference on the number of days and trends of fog at various levels.The HD and FD show no obvious positive correlation until the 1980s.Fog has larger spatial scale,showing more in the south than in the north.Haze occurs mainly around large cities with a discrete distribution.In the background of weakened East Asian Winter Monsoon(EAWM)and sufficient particulate matter,the negative correlation between haze and wind speed is weakened,but the positive correlation between haze and moisture conditions(precipitation and humidity)is significantly strengthened.In recent years,small wind and variability appear frequently.Meanwhile,as the stable source and strong moisture absorption of the aerosol particles,the moisture condition becomes one key control factor in the haze,especially wet haze with less visibility.In contrast,the FD presents a stable positive correlation with precipitation and relative humidity,but has no obvious negative correlation with wind speed. 展开更多
关键词 HAZE FOG VISIBILITY east asian winter monsoon weather conditions
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Degraded Ecosystem and its Rehabilitating Measures in Sandy Areas of North China
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作者 ZHANGFengchun LUQi 《Chinese Forestry Science and Technology》 2004年第4期1-11,共11页
Ecosystem degradation occurs in parallel with desertification process in sandy areas of North China. The vast sandy areas in North China are characterized with flexible environments and fragile ecosystems as well as i... Ecosystem degradation occurs in parallel with desertification process in sandy areas of North China. The vast sandy areas in North China are characterized with flexible environments and fragile ecosystems as well as intensive human activities. Due to the annual precipitation gradient decreases from east to west in North China, the whole sandy region falls into 3 main climatic zones: arid, semi-arid and dry sub-humid zones.The ecosystems in each type of climatic zones are different in climatic conditions, human activities, cultural dimensions, vegetation covers, landscapes, and causes and processes of ecosystem degradation. Therefore, the most effective rehabilitation measures of degraded ecosystems in different types of the climatic zones are also different. For the arid sandy areas, vegetation rehabilitation of degraded ecosystems needs to be completely closed, assisting with artificial measures, such as plantation, irrigation or others. For semi-arid sandy areas, the effective measures of vegetation rehabilitation of degraded ecosystems include increasing of proportion of forests and rangelands and limitation of reclamation; reducing the carrying capacity of livestock on unit area of rangelands and growth of fodder plants; and plantation on the lowlands between sand dunes. For the dry sub-humid areas, the most effective measure is enclosure of degraded ecosystems combined with plantation, and in some cases, just stop uses by grazing or reclamation. 展开更多
关键词 degraded ecosystem DESERTIFICATION REHABILITATION DRYLAND sandy area North China
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