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1)  organic carbon storage
有机碳储量
1.
Soil organic carbon storage and its spatial distribution in Henan Province;
河南省土壤有机碳储量及空间分布
2.
Soil organic carbon storage under different land-use types in Sanjiang Plain
三江平原湿地不同土地利用方式下土壤有机碳储量研究
3.
2%,soil organic carbon storages by 52.
结果表明,从潜在沙漠化到轻度、中度、重度和严重沙漠化,生物量(地上与地下)有机碳储量分别下降26。
2)  Soil organic carbon storage
有机碳储量
1.
The work of estimate soil organic carbon storage is very important to the research of carbon cycle.
结果表明:重庆市20cm和100cm深度的土壤有机碳储量分别为0。
2.
The estimation of soil organic carbon storage is very important to the research of carbon cycle.
结果表明:重庆岩溶区20cm和100cm深度的土壤有机碳储量分别为1。
3)  soil organic carbon storage
土壤有机碳储量
1.
More than 2000 soil samples obtained from the second soil census in China in the year 1998 were applied to analyse the correlations of soil organic carbon storage (SOC) and climatic factors, including annual mean temperature (T), and sum of precipitation (P).
对中国1998年第二次土壤普查中的2000多个土壤剖面中碳储量与年平均温度(T)、年降水量(P) 的相关性研究表明:它们之间的相关性在不同的温度带下具有很大的差异,在T ≤10 oC的地区,土壤有机碳储量与温度的负相关性最强;在10 oC< T ≤20 oC的地区,受与降水正相关的影响,土壤有机碳储量与年平均温度表现出一种正相关性;而在T > 20 oC的地区,土壤有机碳储量与温度和降水的相关性都很差。
2.
Accurate estimation of soil organic carbon storage in the watershed scale ecosystems of arid region is one of the important premise to study the carbon sink and source effect.
研究结果显示,三工河流域0~20 cm土壤有机碳储量为14。
4)  soil organic carbon storage(SOCR)
土壤有机碳储量(SOCR)
5)  organic carbon content
有机碳含量
1.
According to the chemical experimental data of residual organic carbon content,kerogen carbon isotope,aliphaltic gas chromatography/mass spectrometry of 67 outcrop specimens in the Baise basin,the authors analyse the geochemical characteristics of the type and the maturation of organic matter in the Lower Triassic-Devonian source rock.
根据百色盆地周缘大量露头样品的残余有机碳含量、干酪根碳同位素、饱和烃色谱及色质等地球化学实验数据,分析了下三叠统-泥盆系海相烃源岩的有机质丰度、类型、热演化程度。
2.
A usual method for assessing the organic carbon content of source rocks is through a laboratory analyses There is a deviation in calculating organic contents because of non uniform distribution of organic matter.
由于受有机质分布的非均质性和取样人为性等因素的影响,常规的岩心取样分析烃源岩有机碳含量的方法常有一定的偏差。
3.
Taking the mountainous rain forest,secondary Betula alnoides forests with similar age and secondary broadleaved forests as control,the correlation between soil organic carbon content and soil fertility of Betula alnoides plantations located at Puwen experimental forest farm of Xishuangbanna was studied.
在云南西双版纳的普文试验林场,通过对不同龄期西南桦人工纯林林地土壤有机碳含量的比较,并以当地的山地雨林、林龄较为接近的西南桦次生林和黄水(黄牛水+水锦树)次生林林地的土壤有机碳含量为参照,作了对比分析;还对西南桦人工纯林林地土壤的有机碳含量与其土壤肥力状况及物理性状的相关性进行了研究。
6)  TOC
有机碳含量
1.
8%),TOC and hydrocarbon generating potential change insignificantly with increasing maturity.
烃源岩加水热压模拟实验和自然演化剖面实测都表明,海相不同类型烃源岩的有机质丰度热演化可分为3段:未成熟-低成熟阶段(Ro 小于0 8% )随成熟度的增加有机碳含量及生烃潜量变化不明显;在成熟阶段中晚期(Ro 为0 8%~1 3% )有机碳含量和生烃潜量随成熟度增加逐渐降低,其根本原因是油气不断大量生成和排出;在高成熟-过成熟阶段随成熟度的增加有机碳含量变化又不明显。
补充资料:碳标记有机化合物
分子式:
CAS号:

性质:碳标记有机化合物品种很多,常用的多以13CO2和Bal3CO3为起点合成。13CO2与H2在300~350℃ Ni催化剂上反应制13CH4。Bal3CO3与Ba加热生成Bal3C2再与水反应生成13C2H2。LiBH4还原13CO制H13COOH等。

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