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Reconstruction of deep fluid chemical constituents for estimation of geothermal reservoir temperature using chemical geothermometers 利用化学地热计估算地热储层温度的深层流体化学成分重建
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280017
Yanguang Liu, B. Liu, Chuan Lu, Xi Zhu, Guiling Wang
: This paper elaborates the chemical constituent change principles of deep geothermal fluid during the process of upward movement. It summarizes research methods of hydrochemistry, isotope and numerical modelling technique for the physiochemical processes such as decreasing temperature, shallow groundwater infusion, and degassing. The multi-component chemical geothermometry methods including gas geochemical method are discussed. High-temperature geothermal fields in China are mostly located in the southwest with frequent new tectonic movements, especially in Tibet high-temperature geothermal areas. Therefore the paper also focuses the status of high-temperature geothermal fluid research. At last, it ’ s pointed out in the paper that in the future we can start from typical high-temperature geothermal zones and geothermal fields to explore optimization of the multi-component geothermometry method and use it in the reconstruction and analogue of the formation mechanism and internal relevancy of regional geothermal systems.
阐述了深层地热流体在向上运动过程中的化学成分变化规律。总结了水化学、同位素和数值模拟技术在降温、浅层地下水注入、脱气等物理化学过程中的研究方法。讨论了包括气体地球化学方法在内的多组分化学地热测量方法。我国高温地热田多位于新构造运动频繁的西南地区,特别是西藏高温地热区。因此本文还重点介绍了高温地热流体的研究现状。最后指出,今后我们可以从典型的高温地热带和地热田入手,探索多组分地热测量方法的优化,并将其用于区域地热系统形成机制和内部关联性的重建和模拟。
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引用次数: 4
Application of bioremediation in oil contaminated soil 生物修复技术在石油污染土壤中的应用
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280011
Shenmin Zhang, Cuiyun Zhang, Ze He, L. Chen, Miying Yin, Z. Ning, Zhenyang Sun, S. Zhen, F. Zhang
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引用次数: 2
Impact of animal manure addition on the weathering of agricultural lime in acidic soils: The agent of carbonate weathering 添加动物粪便对酸性土壤中农业石灰风化的影响:碳酸盐风化剂
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280020
Zhang Yun, Changli Liu, S. Chao, Hongbing Hou
Fertilization and aglime (agricultural lime) application, as important agricultural activities in acid soil, exert an influence on the fluxes of carbon both between and within ecosystems. Animal manure added to soil can elevate the soil CO2 and release organic acid due to microbial decomposition of the high organic matter content of animal manure. Additionally, the elevated CO2 can accelerate carbonate weathering in alkaline soil, such as lime soil. However, in acidic soil, it is unclear whether the chemical weathering of additive aglime can be quickened by the elevated CO2 due to animal manure addition. Thus, to ascertain the impact of animal manure addition on aglime weathering in acidic soil and to understand the weathering agent of aglime or underlying carbonate in the acidic soil profile, we established two contrasting profiles (control profile and manurial profile) in a cabbage-corn or capsicum-corn rotation in a field experiment site located in the HuaXi district of Guiyang, China, and buried carbonate rock tablets at different depths of soil profiles to calculate the dissolution rate of carbonate rock by monitoring the weights of the tablets. The results indicated that soil CO2 increased due to animal manure addition, but the rate of dissolution of the carbonate rock tablets was reduced, which was attributed to the increase in the pH in acidic soil after animal manure addition because the relationship between the dissolution rate of carbonate rock and soil pH indicated that the weathering rate of carbonate rock was controlled by pH and not by CO2 in acidic soil. Thus, the contribution of H+ ions (mainly exchangeable acid) in acid soil as a weathering agent to the weathering of underlying carbonate (and/or aglime) may lead to the overestimation of the CO2 consumption through chemical weathering at the regional/global scale using hydro-chemical methods.
施肥和施用农业石灰作为酸性土壤中的重要农业活动,对生态系统之间和生态系统内部的碳通量都有影响。添加到土壤中的动物粪便由于微生物分解了动物粪便中的高有机质含量,可以升高土壤CO2并释放有机酸。此外,升高的二氧化碳会加速碱性土壤(如石灰土)中碳酸盐的风化。然而,在酸性土壤中,尚不清楚添加动物粪便引起的CO2升高是否能加速添加剂aglime的化学风化。因此,为了确定添加动物粪便对酸性土壤中aglime风化的影响,并了解aglime或下层碳酸盐在酸性土壤剖面中的风化作用,我们在位于中国贵阳市花溪区的一个田间试验点建立了甘蓝-玉米或辣椒-玉米轮作的两个对比剖面(对照剖面和肥料剖面),并将碳酸盐岩片埋在不同深度的土壤剖面中,通过监测碳酸盐岩片的重量来计算碳酸盐岩的溶解速率。结果表明,添加动物粪便增加了土壤CO2,但碳酸盐岩片的溶解速率降低,这归因于添加动物粪便后酸性土壤中pH的增加,因为碳酸盐岩的溶解速率与土壤pH之间的关系表明碳酸盐岩的风化速率受酸性土壤中的pH控制,而不受CO2控制。因此,酸性土壤中的H+离子(主要是可交换酸)作为风化剂对下层碳酸盐(和/或aglime)风化的贡献可能会导致使用水化学方法在区域/全球范围内通过化学风化高估CO2消耗量。
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引用次数: 1
Study on functions and rational allocation of Shule River Basin groundwater resources 疏勒河流域地下水资源功能及合理配置研究
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280014
Xu Cheng, Xiaoqiong Jin, Wei-po Liu
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引用次数: 0
Determination of organic carbon in soils and sediments in an automatic method 土壤和沉积物中有机碳的自动测定方法
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280012
Guo Li, Lei Yan, Zhimin Chen, Ye Li
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引用次数: 1
Evaluation of groundwater potential and eco-geological environment quality in Sanjiang Plain of Heilongjiang Province 黑龙江省三江平原地下水潜力与生态地质环境质量评价
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280019
Ting-wen Wu, Lihua Wang, Xiang-kui Yang
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引用次数: 3
Scale effects of eroded sediment transport in Wujiang River Basin, Guizhou Province, China 贵州乌江流域侵蚀输沙的规模效应
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280018
Yao Wang, Linming Hou, Yun-long Cai
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引用次数: 3
Hydrogeology of the Ordos Basin, China 鄂尔多斯盆地水文地质
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280010
G. Hou, L. Yin, Dan-dan Xu
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引用次数: 6
Influence of droughts on remote villages in the karst region of Guizhou Province, China: Causes and control 干旱对贵州喀斯特地区偏远村庄的影响:原因与控制
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280009
Yiqun Tang, Qi Yang, Jie Zhou
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引用次数: 0
Risk assessment of heavy metals in topsoil along the banks of theYangtze River in Huangshi, China 黄石市长江沿岸表层土壤重金属风险评价
IF 1.1 4区 地球科学 Q3 Earth and Planetary Sciences Pub Date : 2017-06-01 DOI: 10.26599/jgse.2017.9280016
Lin Dan, Meng-gui Jin, Xiu-Jinz Li
High concentrations of heavy metal in farmland threatens food production and human health. Our study assesses soil quality and the distribution of Cd, Cr, Cu, Zn, Pb and Ni, to identify possible sources of heavy metals along the banks of the Yangtze River in Huangshi. Heavy metal concentrations of 22 topsoil samples were measured using the inductively coupled plasma mass spectrometry instrument and data was analyzed by multivariate statistic approaches. Heavy metal contamination risk assessment was performed using a combination of the Nemerow multi-factor index method, the Hakanson potential ecological risk index method and the Muller index of geo-accumulation method. These methods determined similar results indicating that cadmium (Cd) poses a health risk to residents at the study site while Cr, Cu, Zn, Pb and Ni do not. The Nemerow multi-factor index method demonstrated that 18 samples were heavily polluted, three moderately polluted and one lightly polluted. The Muller index of geo-accumulation method found ten samples were moderately to strongly polluted by Cd, five were moderately polluted, six were lightly to moderately polluted and one was lightly polluted. The Hakanson potential ecological risk index method proved six samples were strongly polluted, seven were moderately polluted and nine were lightly polluted. Since our sampling sites were all in agricultural lands, we recommend the potential ecological risk index method as the most effective given it not only considers the range of pollutants contributing to soil pollution but factors in heavy metals toxicity. We are apt that the source of the high concentrations of Cd found in topsoil is derived from alluvial sediments upstream of the Yangtze River with a high percentage of residual speciation and a low percentage of exchangeable speciation distribution of Cd. This in turns indicates that a high concentration of Cd in soil had little impact on the natural environment. However, 31.9% of the iron-manganese oxides bound speciation indicating that such levels of Cd in soil would be potentially hazardous to the crops, particularly if exposed to a reductive condition.
农田中高浓度的重金属威胁着粮食生产和人类健康。本研究评估了黄石市长江沿岸土壤质量和Cd、Cr、Cu、Zn、Pb和Ni的分布,以确定可能的重金属来源。采用电感耦合等离子体质谱法测定了22个表层土壤样品的重金属浓度,并用多元统计方法对数据进行了分析。采用Nemerow多因素指数法、Hakanson潜在生态风险指数法和Muller地质堆积指数法进行重金属污染风险评价。这些方法得出了相似的结果,表明镉(Cd)对研究地点的居民构成健康风险,而Cr、Cu、Zn、Pb和Ni不构成健康风险。Nemerow多因素指数法结果显示,重度污染18个,中度污染3个,轻度污染1个。地质堆积法Muller指数分析结果显示,Cd污染中至重度污染10份,中度污染5份,轻至中度污染6份,轻度污染1份。Hakanson潜在生态风险指数法证实6个样品为重度污染,7个为中度污染,9个为轻度污染。由于我们的采样点都在农业用地,我们推荐潜在生态风险指数法作为最有效的方法,因为它不仅考虑了造成土壤污染的污染物范围,而且考虑了重金属毒性因素。我们认为,表层土壤中Cd的高浓度来源于长江上游的冲积沉积物,其Cd的残留形态比例较高,而交换形态分布比例较低,这表明土壤中Cd的高浓度对自然环境的影响很小。然而,31.9%的铁锰氧化物结合物种表明,土壤中这样的镉水平对作物有潜在的危害,特别是在暴露于还原性条件下。
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引用次数: 2
期刊
Journal of Groundwater Science and Engineering
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