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Response of Gross Mineralization and Nitrification Rates to Banana Cultivation Sites Converted from Natural Forest in Subtropical China

Author

Listed:
  • Xinghua Qin

    (College of Tropical Crops, Hainan University, Haikou 570228, China)

  • Cheng Yang

    (Geological Survey of Jiangsu Province, Nanjing 210018, China)

  • Lin Yang

    (College of Tropical Crops, Hainan University, Haikou 570228, China)

  • Erdeng Ma

    (Yunnan Academy of Tobacco Agricultural Sciences, Kunming 650021, China)

  • Lei Meng

    (College of Tropical Crops, Hainan University, Haikou 570228, China)

  • Tongbin Zhu

    (Key Laboratory of Karst Dynamics, MRL, Institute of Karst Geology, CAGS, Guilin 541004, China)

Abstract

Evaluations of gross mineralization (M Norg ) and nitrification (O NH4 ) can be used to evaluate the supply capacity of inorganic N, which is crucial in determining appropriate N fertilizer application. However, the relevant research for banana plantations to date is limited. In this study, natural forest and banana plantations with different cultivation ages (3, 7, 10, and 22 y) were chosen in a subtropical region, and the 15 N dilution technique was used to determine the gross M Norg and O NH4 rates. The objective was to evaluate the effect of the conversion of natural forests to banana plantations on inorganic N supply capacity (M Norg + O NH4 ) and other relevant factors. Compared to other natural forests in tropical and subtropical regions reported on by previous studies, the natural forest in this study was characterized by a relatively low M Norg rate and a high O NH4 rate in the soil, resulting in the presence of inorganic N dominated by nitrate. Compared to the natural forest, 3 y banana cultivation increased the M Norg and O NH4 rates and inorganic N availability in the soil, but these rates were significantly reduced with prolonged banana cultivation. Furthermore, the mean residence times of ammonium and nitrate were shorter in the 3 y than in the 7, 10, and 22 y banana plantations, indicating a reduced turnover of ammonium and nitrate in soil subjected to long-term banana cultivation. In addition, the conversion of natural forest to banana plantation reduced the soil organic carbon (SOC), total N and calcium concentrations, as well as water holding capacity (WHC), cation exchangeable capacity (CEC), and pH, more obviously in soils subjected to long-term banana cultivation. The M Norg and O NH4 rates were significantly and positively related to the SOC and TN concentrations, as well as the WHC and CEC, suggesting that the decline in soil quality after long-term banana cultivation could significantly inhibit M Norg and O NH4 rates, thus reducing inorganic N supply and turnover. Increasing the amount of soil organic matter may be an effective measure for stimulating N cycling for long-term banana cultivation.

Suggested Citation

  • Xinghua Qin & Cheng Yang & Lin Yang & Erdeng Ma & Lei Meng & Tongbin Zhu, 2021. "Response of Gross Mineralization and Nitrification Rates to Banana Cultivation Sites Converted from Natural Forest in Subtropical China," Land, MDPI, vol. 10(4), pages 1-12, April.
  • Handle: RePEc:gam:jlands:v:10:y:2021:i:4:p:376-:d:530144
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    References listed on IDEAS

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    1. Zihan Jiang & Hongyan Liu & Hongya Wang & Jian Peng & Jeroen Meersmans & Sophie M. Green & Timothy A. Quine & Xiuchen Wu & Zhaoliang Song, 2020. "Bedrock geochemistry influences vegetation growth by regulating the regolith water holding capacity," Nature Communications, Nature, vol. 11(1), pages 1-9, December.
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    Cited by:

    1. Lin Yang & Xuebin Zhang & Jinxia Liu & Dongni Wen & Lei Meng & Tongbin Zhu, 2022. "Divergent Response of the Supply Capacity and Turnover of Inorganic Nitrogen to Pitaya Cultivation in the Subtropical Karst Region of Southwest China," Land, MDPI, vol. 11(6), pages 1-11, May.

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