International Journal of Applied Science and Engineering
Published by Chaoyang University of Technology

Muhamad Khairulamiin Md Taha1, Azham Mohamad2*, Intan Soraya Che Sulaiman3, Isharudin Md Isa4, Mohd Nizar Khairuddin5

1 Department of Crop Science, Faculty of Agriculture and Food Sciences, Universiti Putra Malaysia Bintulu Campus, 97008 Bintulu, Sarawak, Malaysia

2 Centre of Foundation Studies for Agricultural Science, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia

3 Faculty of Applied Sciences, Universiti Technologi Mara, Perlis Branch, Arau Campus, 02600, Arau, Perlis, Malaysia

4 Department of Crop Science, Faculty of Agriculture, Universiti Putra Malaysia, 43400 UPM Serdang, Selangor, Malaysia

5 Department of Statistics, FGV R&D Sdn. Bhd., Tun Razak Center of Agriculture Research, 26400 Bandar Tun Abdul Razak Jengka, Malaysia


 

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ABSTRACT


Recovery of soil organic matter and mineral nutrient cycling are critical to the success of rehabilitation process of replanted forest. We investigated the dynamic changes in soil of selected physicochemical properties including organic carbon (C), nitrogen (N), phosphorus (P) and sulphur (S) of replanted forest rehabilitation that had been previously disturbed by anthropogenic activities. Soil samples were collected from the rehabilitated forest of three ages stands (3-, 12- and 23-years old) while samples from adjacent secondary forest was collected for comparison. Altogether, 36 samples were taken randomly with a soil auger at depths of 0-20 cm from a plot of 20 × 20 m2 at each site. Soils were analyzed for pH, bulk density, C, N, P and S. The data obtained were statistically analyzed using ANOVA with Tukey’s test performed by SAS 9.2 at P ≤ 0.05. Results showed that total C, N, P, C/N ratio and C/S ratio increased with age of rehabilitated forest except for pH, S and C/P ratio. Forest rehabilitation by planting indigenous tree species has shown a potential of recovery, but further investigation into the process control of the dynamic changes of soil physicochemical properties, particularly in the event of further ecosystem disturbance is needed.


Keywords: Forest resilience, Soil carbon, Replanted tropical forest.


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REFERENCES


  1. Ahmed, O.H., Ch’ng, Y.H., Majid, N.M.A. 2012. Rehabilitation of degraded Malaysian tropical forest and soil carbon storage. UPM Press. UPM. Serdang.

  2. Brady, N.C., Weil, R.R. 2008. The nature and properties of soils 13th edition. Prentice Hall. New Jersey.

  3. Catherine, P., Rock, O. 2008. Organic carbon, organic matter and bulk density relationships in boreal forest soils. Canadian Journal of Soil Science. 88, 315–325.

  4. FAO. 1995. Forest resources assessment 1990. Global synthesis. FAO Forestry paper 124. Rome, Italy.

  5. FAO. 2001. Global forest resources assessment 2000. Main report. FAO Forestry paper 140, Rome, Italy.

  6. Gajić, B. 2013. Physical properties and organic matter of fluvisols under forest, grassland, and 100 years of conventional tillage. Geoderma 200,114–119.

  7. Holl, K.D., Aide, T.M. 2011. When and where to actively restore ecosystems? Forest ecology and management, 261, 1558–1563.

  8. Holl, K.D. 1999. Factors limiting tropical rain forest regeneration in abandoned pasture: seed rain, seed germination, microclimate, and soil. 31, 229–242.

  9. Kavian, A., Azmoodeh, A., Solaimani, K. 2014. Deforestation effects on soil properties, runoff and erosion in northern Iran. Arabian Journal of Geosciences, 7, 1941–1950.

  10. Kimble, J.M., Heath, L.S., Birdsey, R.A., Lal, R. 2003. The potential of U.S. forest soils to sequester carbon and mitigate the greenhouse effect. Lewis Publisher. U.S.A.

  11. Lal, R. 1987. Managing the soils of sub-Saharan Africa. Science, 236, 1069–1076.

  12. Lal, R. 1997. Degradation and resilience of soils. Philosophical Transactions of The Royal Society Biological Sciences, 352, 997–1010.

  13. McDonald, M.A., Healey, J.R., Stevens, P.A. 2002. The effects of secondary forest clearance and subsequent land use on erosion losses and soil properties in the Blue Mountains of Jamaica. Agriculture Ecosystems and Environment, 92, 1–19.

  14. Peech, M. 1965. Hydrogen‐ion activity. Methods of Soil Analysis: Part 2 Chemical and Microbiological Properties, 9, 914–926.

  15. Pimm, S.L. 1984. The complexity and stability of ecosystems. Nature, 307, 321–326.

  16. Schroth, G., Sinclair, F. L. (Eds.). 2003. Trees, crops, and soil fertility: concepts and research methods. Cabi. 77–89.

  17. Seybold, C.A., Herrick, J.E., Brejda, J.J. 1999. Soil resilience: A fundamental component of soil quality, Soil Science, 164, 224–234.

  18. Vitousek, P.M., Matson, P.A., Van Cleve, K. 1989. Nitrogen availability and nitrification during succession: Primary, secondary, and old-field series. Plant Soil,115, 229–239

  19. Vitousek, P.M. 1984. Litterfall, nutrient cycling, and nutrient limitation in tropical forests. Ecology, 65, 285–298.

  20. Young, A. 2003. Agroforestry for soil management 2nd Edition. CAB International, Kenya.


ARTICLE INFORMATION


Received: 2021-07-14
Revised: 2022-06-08
Accepted: 2022-07-18
Available Online: 2022-11-28


Cite this article:

Taha, M.K.M., Mohamad, A., Sulaiman, I.S.C., Isa, I.M., Khairuddin, M.N. Monitoring soil resilience via the dynamic changes of selected physicochemical properties of soil in a tropical rehabilitated forest. International Journal of Applied Science and Engineering, 19, 2021267https://doi.org/10.6703/IJASE.202212_19(4).005

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