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91.
在我国改革开放政策实行较早的广东珠江三角洲地区,我们对地处西南部的新会市进行了为期两年的全面、典型抽样调查。发现全市的耕地面积和播种面积呈下降趋势,单产虽有较大幅度的增长但粮食总产量的增长缓慢,速度低于全市总人口的自然增长率,因此人均粮食产量呈下降趋势。根据建立的灰色GM(1,1)模型预测,新会市2010年人均耕地面积只有0.025hm^2,在“人均4分保命田”之下。因此,本文对该地区作出的粮食及 相似文献
92.
The water quality of Dianchi Lake declines quickly and the eutrophication is getting serious. To identify the internal pollution
load of Dianchi Lake it is necessary to evaluate its sediment accumulation. Sedimentation rates of Dianchi Lake are determined
by 137Cs dating. However, 137Cs vertical distribution in sediment cores of Dianchi Lake has special characteristics because Dianchi Lake is located on
the southeast of the Qinghai-Tibet Plateau, the Kunming quasi-stationary front is over the borders of Yunnan and Guizhou where
the specific precipitation is distributed. Besides 1954, 1963 and 1986 137Cs marks can be determined in sediment cores, a 137Cs mark of 1976 representing the major period of 137Cs released from China unclear test can be determined and used for an auxiliary dating mark. Meanwhile Dianchi Lake is divided
into seven sections based on the water depth, basin topography, hydrological features and supplies of silt and the lakebed
area of each section is calculated. The mean annual sedimentation rates for seven sections are 0.0810, 0.1352, 0.1457, 0.1333,
0.0904, 0.1267 and 0.1023 g/cm2a in 1963–2003, respectively. The gross sediment accumulation of the lake is 26.18×104 t/a in recent 17 years and 39.86×104 t/a in recent 50 years.
Foundation: National Natural Science Foundation of China, No.40771186; The Key Project of the State Key Laboratory of Soil Sustainable
Agriculture, Nanjing Institute of Soil Sciences, Chinese Academy of Sciences, No.5022505
Author: Zhang Yan (1962–), Ph.D and Associate Professor, specialized in environmental change. 相似文献
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Jingen Dai Chengshan Wang Réjean Hébert Yalin Li Hanting Zhong Raoult Guillaume Rachel Bezard Yushuai Wei 《Gondwana Research》2011,19(1):232-243
The Yarlung Zangbo Suture Zone (YZSZ) is believed to be composed of material largely derived from the destruction of the Neo-Tethys that occurred from early Mesozoic to early Cenozoic. We report here geochronological and petrological data obtained for newly discovered alkaline gabbro blocks embedded in a mélange zone of the western YZSZ. Single zircon U–Pb analyses from one representative gabbro sample by SIMS (Secondary Ion Mass Spectrometry) yielded a combined crystallization age of about 363.7 ± 1.7 Ma (1σ). In situ Hf isotopic analyses yielded εHf(t) values of + 2.6 to + 5.5, suggesting an enriched mantle source. All of the gabbro samples show typical Ocean Island Basalt (OIB) affinity with little or no continental crust contamination. They also display strong geochemical similarities with the Hawaii basalts and the Xigaze seamount basalts suggestive of their intra-oceanic setting. These observations, in combination with the Early Carboniferous layered gabbros reported at Luobusa, indicate that these rocks could represent remnants of the Paleo-Tethys. We propose that a branch ocean separating the Western Qiangtang terrane and the Lhasa terrane from the Gondwana continent might have been present during the Late Devonian and the Early Carboniferous, providing new constrains on the configuration of Paleo-Tethys in Tibetan Plateau during early Late Paleozoic. 相似文献
97.
In dam safety assessment, it is customary to focus on stability analysis, and the safety factor is regarded as an assessment
index that cannot correctly reflect the effect of multi-factors and variable uncertainty. The factors that induce dam breaks
are complex and uncertain; however, three primary ones can be identified: hydrological factors, seepage and bank slope instability.
In this paper, the risk probability and the dam break threshold value for each factor individually, as well as coupled factors,
are studied. The threshold value is acquired using the relationship formula between risk probability and dam type. The Dongwushi
reservoir located in the Hebei province of China is taken as a case study. The results show that the dam break threshold values
for hydrological factors, seepage and bank slope instability are 2.53, 2.02 and 2.69, respectively. The integrated dam break
threshold value for the coupled factors is 1.25, which indicates that the dam is under serious stress according to the established
risk assessment standard. The safety factor is calculated as 1.15 using the Bishop method, which indicates that the dam is
under serious stress. The results obtained by the proposed method are consistent with those of the Bishop method. Finally,
the proposed theory and method are introduced into a dam safety evaluation system (DSES) for convenient and efficient dam
safety management. 相似文献
98.
中国东部土壤温度、湿度变化的长期趋势及其与气候背景的联系 总被引:2,自引:0,他引:2
利用1971—2000年中国722站逐月的土壤温度资料和1981—1998年178站逐旬的土壤湿度观测资料,分析了中国东部土壤温度、湿度变化的长期趋势及其与气温、降水变化的关系。结果表明:①我国东部土壤温度的变化在年际—年代际时间尺度上存在明显的区域性差异,其中东北地区表现为持续上升型,而西北东部—华北、江淮和西南—华南地区均为先降后升型;②1970—2000年代,土壤温度的变化在东北以及西北东部—华北地区有显著的上升趋势,而在江淮和西南—华南地区,总体而言变化趋势不显著。此外,1980—1990年代,各区域土壤湿度的变化趋势均不显著;③在年际—年代际尺度上,各区域土壤温度和气温的变化具有显著的正相关关系,而土壤湿度与土壤温度的变化普遍呈负相关关系,其中尤以西北东部—华北地区最为显著。而在较长的时间尺度上,土壤湿度与降水的变化仍然存在较好的正相关关系。 相似文献
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