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Volume 37 Issue 5
Oct.  2018
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Article Navigation >  CARSOLOGICA SINICA  > 2018  >  37(5): 770-776
WANG Jiangnan, FENG Huoju, LI Baiqiu, FANG Kai, SHI Jianmin. Distribution, transportation and accumulation of mineral elements in a rock-soil-plant system of Phyllostachys glauca in limestone mountains[J]. CARSOLOGICA SINICA, 2018, 37(5): 770-776. doi: 10.11932/karst20180515
Citation: WANG Jiangnan, FENG Huoju, LI Baiqiu, FANG Kai, SHI Jianmin. Distribution, transportation and accumulation of mineral elements in a rock-soil-plant system of Phyllostachys glauca in limestone mountains[J]. CARSOLOGICA SINICA, 2018, 37(5): 770-776. doi: 10.11932/karst20180515
shu

Distribution, transportation and accumulation of mineral elements in a rock-soil-plant system of Phyllostachys glauca in limestone mountains

doi: 10.11932/karst20180515
  • 1.

    College of Forestry, Jiangxi Agricultural University, Nanchang, Jiangxi 330045, China/Jiangxi Provincial Key Laboratory for Bamboo Germplasm Resources and Utilization, Nanchang, Jiangxi 330045, China

  • 2.

    Ruichang Bureau of Forestry, Ruichang, Jiangxi 333200, China

  • 3.

    Jiangxi Institute of Geological Survey, Nanchang, Jiangxi 330030, China

  • Publish Date: 2018-10-25
    Abstract
  • Discerning the transportation and accumulation of mineral elements in rock-soil-plant systems permits to guide the vegetation restoration in karst ecosystems. Rock, soil and four plant species including one dominant species Phyllostachys glauca, three auxiliary species Elaeagnus pungens, Camellia oleifera and Ilex cornutawere sampled in limestone mountains of Ruichang city, Jiangxi Province, China. Nine mineral elements (N, P, K, Ca, Mg, Fe, Al, Mn, Na) were determined for the rock, soil and plant samples, and the characteristics of transportation and accumulation of these elements were analyzed. The results show that(1) the limestone in the Ph. glauca forest is high in Ca concentration (363.09 g· kg-1); the soil concentration of Ca (2.68 g·kg-1) and Mg (5.94 g· kg-1) are low, while the concentrations of Fe and Al are high with the values of 48.12 g· kg-1and 84.00 g· kg-1, respectively. The content of N, P and Ca in plant is higher than that in soil, the vice verse for other elements. (2) From rock to soil, Ca is largely lost by leaching with a transport coefficient of 0.01, while other elements are all accumulated. Fe and Al are in the top of transport coefficient rank with values of 9.98 and 14.10, respectively. From soil to plant, only N, Ca and P are accumulated in plants, and the content of other elements in plants is lower than that of in soil. The bio absorption coefficients of Fe and Al are very low with values of 1.41 and 2.08, respectively. (3) The element concentration and biological absorption coefficients of Ph. glauca are lower than that of three auxiliary species with the exception of element K. It indicates that limestone has developed into terra rossa under strong leaching. The four species growing in the terra rossa are all not calciphytes. The transportation and accumulation of mineral elements in the rock-soil-plant system change the different soil formation processes and plant species. Less element absorption of Ph. glauca may be the physiological basis for its domination in the limestone habitat.

     

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