SPATIOTEMPORAL VARIABILITY OF ERODED ORGANIC MATTER, NITROGEN, AND NITRATE IN RESPONSE TO MONSOONAL CHANGES IN A BLACK PEPPER FARM

Authors

  • Izzah Abd Hamid Department of Crop Science, Faculty of Agricultural and Forestry Sciences, Universiti Putra Malaysia Bintulu Sarawak Campus, 97008 Bintulu, Sarawak, Malaysia
  • Wan Asrina Wan Yahaya Department of Crop Science, Faculty of Agricultural and Forestry Sciences, Universiti Putra Malaysia Bintulu Sarawak Campus, 97008 Bintulu, Sarawak, Malaysia
  • Samsuri Abdul Wahid Department of Land Management, Faculty of Agriculture, Universiti Putra Malaysia, 43400 Serdang, Selangor, Malaysia
  • Wan Mohd Razi Idris Department of Earth Sciences and Environment, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600, Bangi, Selangor, Malaysia

DOI:

https://doi.org/10.11113/jurnalteknologi.v88.21611

Keywords:

Vegetative cover, tropical monsoon climate, monsoon rainfall, coarse-textured soil, sloping terrain

Abstract

Organic matter (OM), total nitrogen (N), and nitrate (NO3) play a significant role in soil fertility and are critical for the black pepper industry. Hence, the objectives of this study were to analyse the spatiotemporal variability and inter-relationships among OM, N, and NO3 concerning fluctuations brought about by monsoonal changes. A total of 264 soil samples were collected across four monsoonal periods: Inter-April (Inter-Apr.), Southwest monsoon, Inter-October (Inter-Oct.), and Northeast monsoon. Descriptive statistics, Pearson correlation, and geostatistical techniques (Ordinary Kriging and semivariogram modelling) were employed to assess the spatial distribution and variability of these nutrients. The findings of this study revealed that the movement of OM, N, and NO3 was heavily affected by monsoonal transitions and further expedited by multifarious factors, such as steep terrain (26°), textural class (>78.49% sand), crop coverage (35.06%), and farm management. OM, N, and NO3 concentrations showed significant variations across monsoonal periods, with OM increasing by 24.3% and N by 22.1% during the Southwest monsoon, while NO3 exhibited an 86.0% rise. However, NO3 declined by 53.0% during the subsequent transition to the Northeast monsoon, coinciding with high rainfall (1,223 mm). Spatial dependence varied, with OM exhibiting moderate dependence (27.175%) and NO3 showing weak spatial dependence (<3%). Frequent rainfall and nutrient insufficiency led to distinct distribution patterns, characterised by reduced spatial dependency and variability during the Northeast monsoon. Meanwhile, the Southwest monsoon had the capacity to retain NO3 temporarily within the soil due to limited moisture availability. 

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Published

2025-12-23

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Science and Engineering