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weathering flux
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  侵蚀通量
     The weathering flux of organic carbon in Xijiang River drainage area is about 10.18×10 6gC/km 2·yr.
     西江流域的有机碳侵蚀通量为 10 .18× 10 6gC/km2 ·yr.
短句来源
     , which is two to three times in quantiy of the average value in the global external drainage area. The POC is the main constitute of the riverine organic carbon, which weathering flux is about 8.30×10 6gC/km 2·yr.
     ,是全球外流域有机碳侵蚀通量的 2~ 3倍 ,其中以颗粒有机碳的侵蚀通量为主 ,达到 8.30× 10 6gC/km2 ·yr.
短句来源
     The weathering flux of dissolved organic carbon is about 1.88×10 6gC/km 2·yr.
     ,溶解有机碳的侵蚀通量为 1.88× 10 6gC/km2 ·yr . 。
短句来源
     The weathering flux of organic carbon in Beijiang River drainage basin is about 10 01×10 6g·km -2 ·a -1 , which is constituted by 6 54×10 6g·km -2 ·a -1 of POC and 3 47×10 6g·km -2 ·a -1 of DOC. This pattern of organic carbon weathering flux in Beijiang drainage basin is consistent with that of most of the monsoon drainage basins.
     初步估算 ,北江流域的有机碳侵蚀通量为 1 0 0 1× 1 0 6g·km- 2 ·a- 1,其中以颗粒有机碳为主 ,达到 6.54× 1 0 6g·km- 2 ·a- 1,溶解有机碳的侵蚀通量为3 4 7× 1 0 6g·km- 2 ·a- 1.北江流域有机碳侵蚀通量的总量和组成特点与多数季风流域具有更大的一致性 .
短句来源
  相似匹配句对
     ON THUNDERSTORM WEATHERING
     论雷暴风化作用
短句来源
     On the Teaching of Flux
     关于通量的教学
短句来源
     Life in Flux
     流动中的生命
短句来源
     Weathering of Ware Glasses
     器皿玻璃的风化
短句来源
     The weathering flux of dissolved organic carbon is about 1.88×10 6gC/km 2·yr.
     ,溶解有机碳的侵蚀通量为 1.88× 10 6gC/km2 ·yr . 。
短句来源
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  weathering flux
Our results suggest that under a specific vegetative cover, the soil carbon environment affects the weathering flux observed.
      
We substitute overall weathering flux F0 w for soil erosion rate in the LO model.
      
We substitute 253overall weathering flux F 0 w for soil erosion rate in the LO 254model.
      
Testing the model sensitivity to changes in weathering flux indicates that small changes result in considerable variation in atmospheric O2.
      
In the modern oceans 30 percent of the total weathering flux of Ca plus Mg consists of Mg.
      
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Riverine water samples were collected from the lower reach hydrometric station of Xijiang River, namely Makou, in four hydrological seasons. The samples were analyzed of their organic carbon. The analysis results demonstrated that the distribution of organic carbon, including particulate organic carbon (POC) and dissolved organic carbon (DOC), is fairly suitable in the sampling section in every season. The contents of organic carbon and total suspended substance (TSS) in riverine water body varied seasonally...

Riverine water samples were collected from the lower reach hydrometric station of Xijiang River, namely Makou, in four hydrological seasons. The samples were analyzed of their organic carbon. The analysis results demonstrated that the distribution of organic carbon, including particulate organic carbon (POC) and dissolved organic carbon (DOC), is fairly suitable in the sampling section in every season. The contents of organic carbon and total suspended substance (TSS) in riverine water body varied seasonally with the discharge in a positive pattern. With the content of total suspended substances increasing, the quality partition of organic carbon in TSS decreased in a logarithm tendency. The weathering flux of organic carbon in Xijiang River drainage area is about 10.18×10 6gC/km 2·yr., which is two to three times in quantiy of the average value in the global external drainage area. The POC is the main constitute of the riverine organic carbon, which weathering flux is about 8.30×10 6gC/km 2·yr. The weathering flux of dissolved organic carbon is about 1.88×10 6gC/km 2·yr. The mechanical erosion is very intense in this drainage area, which is considered to be related to the typical monsoon climate and to the comparatively great undulation of the landforms in this drainage basin. The long history and fairly intense utility of the land for agriculture use are all responsible for the serious soil erosion in this area.

在西江下游的马口水文站对径流进行了 4个季节的有机碳采样分析。研究表明 ,西江径流有机碳的断面构成在各个季节均较为一致 ;季节性变化表现为 ,有机碳和悬浮物含量随流量的增加而增加。随着水体悬浮物含量的增加 ,悬浮物的有机碳含量呈对数趋势降低。西江流域的有机碳侵蚀通量为 10 .18× 10 6gC/km2 ·yr.,是全球外流域有机碳侵蚀通量的 2~ 3倍 ,其中以颗粒有机碳的侵蚀通量为主 ,达到 8.30× 10 6gC/km2 ·yr.,溶解有机碳的侵蚀通量为 1.88× 10 6gC/km2 ·yr .。反映了流域内较强的机械剥蚀过程 ,这与西江流域典型的季风气候、较大的地形高差 ,以及农业耕作历史长久、土地利用强度较大等因素有关。

Riverine water samples were collected from Hekou hydrometric station of Beijiang River in five hydrological seasons. The samples were analyzed of their organic carbon and total suspended substance, which demonstrated that the concentrations of particulate organic carbon (POC) changed synchronically with the concentrations of total suspended substance (TSS) in riverine water. The correlation between the concentrations of TSS and dissolved organic carbon (DOC), however, is sometimes positive and sometimes negative,...

Riverine water samples were collected from Hekou hydrometric station of Beijiang River in five hydrological seasons. The samples were analyzed of their organic carbon and total suspended substance, which demonstrated that the concentrations of particulate organic carbon (POC) changed synchronically with the concentrations of total suspended substance (TSS) in riverine water. The correlation between the concentrations of TSS and dissolved organic carbon (DOC), however, is sometimes positive and sometimes negative, and the correlation is not so notable as that between TSS and POC. With the concentration of total suspended substances increasing, the quality partition of organic carbon in total suspended substance decreased in a logarithm tendency. The transportation of organic carbon, especially of DOC, mainly takes place in flood peak periods. The weathering flux of organic carbon in Beijiang River drainage basin is about 10 01×10 6g·km -2 ·a -1 , which is constituted by 6 54×10 6g·km -2 ·a -1 of POC and 3 47×10 6g·km -2 ·a -1 of DOC. This pattern of organic carbon weathering flux in Beijiang drainage basin is consistent with that of most of the monsoon drainage basins.

选取北江的河口站断面 ,对径流进行了 5个季节的采样分析 .结果表明 ,北江径流中颗粒有机碳含量随总悬浮物含量的变化而同步变化 ;溶解有机碳含量与总悬浮物含量之间有时表现微弱的正相关 ,有时表现微弱的负相关 .随着水体总悬浮物含量的增加 ,总悬浮物中有机碳的质量分数呈对数趋势降低 .洪峰时期径流对有机碳的搬运是全年总搬运量的主要部分 ,这种现象对于溶解有机碳更为显著 .初步估算 ,北江流域的有机碳侵蚀通量为 1 0 0 1× 1 0 6g·km- 2 ·a- 1,其中以颗粒有机碳为主 ,达到 6.54× 1 0 6g·km- 2 ·a- 1,溶解有机碳的侵蚀通量为3 4 7× 1 0 6g·km- 2 ·a- 1.北江流域有机碳侵蚀通量的总量和组成特点与多数季风流域具有更大的一致性 .

 
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