Volume 46 Issue 7
Jul.  2021
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Article Navigation >  Earth Science  > 2021  >  46(7): 2621-2645
Sun Houyun, Wei Xiaofeng, Sun Xiaoming, Jia Fengchao, Li Duojie, Li Jian, 2021. Element Migration and Accumulation Characteristics of Bedrock-Regolith-Soil-Fruit Plant Continuum of the Earth's Critical Zone in Chengde Almond Producing Area. Earth Science, 46(7): 2621-2645. doi: 10.3799/dqkx.2020.285
Citation: Sun Houyun, Wei Xiaofeng, Sun Xiaoming, Jia Fengchao, Li Duojie, Li Jian, 2021. Element Migration and Accumulation Characteristics of Bedrock-Regolith-Soil-Fruit Plant Continuum of the Earth's Critical Zone in Chengde Almond Producing Area. Earth Science, 46(7): 2621-2645. doi: 10.3799/dqkx.2020.285
shu

Element Migration and Accumulation Characteristics of Bedrock-Regolith-Soil-Fruit Plant Continuum of the Earth's Critical Zone in Chengde Almond Producing Area

doi: 10.3799/dqkx.2020.285
  • 1.

    School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China

  • 2.

    Beijing Institute of Geology for Mineral Resources, Beijing 100012, China

  • 3.

    China Institute of Geo-Environment Monitoring, Beijing 100081, China

  • Received Date: 2020-10-05
  • Publish Date: 2021-07-15
    Abstract
  • Eco-geochemical conditions have an important impact on the quality of characteristic crops. It is of great significance to carry out investigation of the element migration and accumulation characteristics of the bedrock-regolith-soil-plant continuum of the Earth's critical zone for the adaptive evaluation on agricultural planting and the optimization of utilization of agricultural land. Taking the almond producing area in Chengde, Hebei Province as the study area, the quantitative evaluation of element migration in BRSPC was calculated by multiple chemical weathering index, chemical depletion fraction, mass transfer coefficient and bioconcentration factor in clastic rock and volcanic rock formation area combining multiple statistical methods. The results indicate that the element geochemical grade of TK and TFe2O3 were categorized as rich level, Se categorized as moderate level, Cu and Ge categorized as moderate-rich level and TP, TS, B as insufficient level. The bedrock-regolith-soil samples in the study area are generally at the elementary chemical weathering stage while the weathering intensity of soil ofvolcanic rock formation area is relatively higher than that of clastic rock formation area. The TS, B, Se, Ti, MgO and Fe2O3 contents are relatively enriched in soil during the weathering process of bedrocks, and the Se, S, B, Ni, and V are strong active elements for mass migration. The Se content of 85.71% of the almond pulp samples belong to the selenium-rich fruit, with 25% of the almond samples being above the selenium-enriched level. Meanwhile, The Se content in both of almond pulp and almond samples located in clastic rock formation are relatively higher than that in volcanic rock formation. The characteristics of element enrichment and loss in weathering process are closely related to the element migration in the soil-plant absorption process, and the bedrock-regolith-soil-plant continuum has a good inheritance on element conduction. The contents of Cu, Zn, TP, Se, B, Cao and TFe2O3 in soil were the main geochemistry factors restricting the quality of almond and pulp in the study area. The leaching loss of Cu and Zn elements in the weathering process of volcanic bedrock is greater than that in clastic rock area, while the contents of TP, Se, B, Cao and TFe2O3 in the soil of clastic rock formation area are higher than those in the volcanic rock formation area, which leads to the conclusion that the clastic rock formation area is more suitable for almond apricot planting.

     

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