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Article

Variations in the Forest Productivity of Pinus patula Plantations in Tanzania: The Need for an Improved Site Classification System

by
Joshua Maguzu
1,*,
Ulrik Ilstedt
2,
Josiah Zephaniah Katani
3 and
Salim S. M. Maliondo
4
1
Regional Research School in Forest Sciences (REFOREST), College of Forestry, Wildlife and Tourism College of Forestry, Wildlife and Tourism, Sokoine University of Agriculture, Morogoro P.O. Box 3009, Tanzania
2
Department of Forest Ecology and Management, Swedish University of Agriculture Science, Skogsmarksgränd, 901 83 Umeå, Sweden
3
Department of Forest Resource Assessment and Management, Sokoine University of Agriculture, Morogoro P.O. Box 3013, Tanzania
4
Department of Forest Biology, Sokoine University of Agriculture, Morogoro P.O. Box 3010, Tanzania
*
Author to whom correspondence should be addressed.
Forests 2024, 15(7), 1247; https://doi.org/10.3390/f15071247
Submission received: 6 June 2024 / Revised: 5 July 2024 / Accepted: 8 July 2024 / Published: 18 July 2024
(This article belongs to the Special Issue Forest Growth and Yield under Environmental Changes)

Abstract

:
The productivity of forests in sub-Saharan Africa is often summarized into large compartments or site classes. However, the classification of forest productivity levels based on the original site index model in Tanzania and the techniques applied to generate the model did not include the micro-toposequence variations within compartments. This may create false expectations of wood supply and hinder the estimation of sustainable harvesting processes. This study analyzed variations in forest productivity and the site index in P. patula stands in two forest plantations of Tanzania to assess the applicability and generality of the present site classification system. We used dominant height as a proxy for forest productivity in 48 plots at the Sao Hill forest plantation (SHFP) and 24 plots at the Shume forest plantation (SFP). We stratified the sampling plots in each site class along the soil catena and recorded the elevation, slope, and slope positions (summit, mid, and lower). Our results showed that the site classes did not generally match the previously assigned site classes and the productivity of a given site class varied between the two plantations. We found a consistently higher productivity than that implied by the original site index in SFP, while in SHFP, the productivity was both higher and lower than estimated in different compartments. Both elevations and slope significantly contributed to predicting the productivity variations within site classes. Overall, the results indicate that physiographic factors affect variations in forest productivity within the assigned site classes. We recommend a more comprehensive site productivity assessment that takes into account physiographic variations and hence provides more accurate information for sustainable forest plantation management in Tanzania and in the region at large.

1. Introduction

Forest plantations were estimated to cover over 294 million ha by 2022 [1] and have been established to meet the increasing global demand for timber products [2,3]. Such plantations have the potential to supply the world with its entire wood needs [4,5,6]. However, the productivity of tropical forest plantations grown on short- to medium-term rotation lengths can vary significantly. Globally, the production of wood products in 2020 totaled 473 million m3 of sawn wood, 368 million m3 of wood-based panels, and 401 million tonnes of paper and paperboard [7]. The global demand for timber has seen a significant increase of over 30% in the last 10–20 years, driven by economic development, urbanization, and climate change mitigation efforts that rely on timber as a renewable resource [8]. Therefore, to be able to match wood demand, production, and plantation areas at the global, regional, and local scales, timely and accurate information on the productivity of plantation forests is essential [9].
Pinus patula is a forest tree species native to Mexico, widely cultivated in tropical and subtropical regions of the world [10]. In its natural range, P. patula grows from 18° to 24° North latitude and from 1800 to 2700 m above sea level. Its rainfall range is from a 750 to 2000 mm annual average. The species is largely used for plantations in tropical and subtropical regions of the world, including South America, Central and Southern Africa, Indonesia, Australia, and New Zealand [11]. The area of planted P. patula worldwide is approximately 1 million hectares, of which 95% corresponds to plantations in central, eastern, and southern Africa [11,12]. In Africa, plantations of this species have gained considerable interest, being represented in different African countries and probably being the most widely planted pine in tropical Africa. The demand for P. patula timber has increased in the last 10–20 years due to improvements in economic well-being and population growth, which have driven up the overall consumption of wood-based products.
The productivity of forests varies significantly, with the mean annual increment (MAI) ranging from as low as 1–2 m3 ha−1 yr−1 to as high as 25–30 m3 ha−1 yr−1 [13]. Eucalypts and tropical pines are the primary species in tropical timber plantations [13]. In southern Africa, the productivity of P. patula ranges from 18 to 28 m3 ha−1 yr−1 [10]. In South Africa, P. patula planted in well-drained soils is expected to have a MAI range of 11 to 27 m3 ha−1 yr−1, with good stem form and wood properties [14]. Several factors can affect forest productivity, such as site quality, age, silviculture, type of planting materials, species, irradiance, physiography, and stable environmental factors like edaphic and micro-climatic factors [15,16,17,18]. Understanding forest productivity is crucial for sustainable forest management, as it helps land managers make informed decisions about species selection, rotation lengths, and silvicultural treatments [13].
Physiographic factors, including elevation, aspect, and slope, influence plant growth [19]. The effect of elevation and slope on forests has been widely studied [20], as they can be valuable indicators of the distribution of environmental conditions such as radiation, precipitation, temperature, and soil water and nutrient availability [21,22] that affect the composition and productivity of a species [23]. The effect of physiographic factors on forest productivity is closely linked with soil physical and chemical properties including soil depth, aeration, and nutrient and water availability [24]. Thus, differences in site conditions can result in variations in site index predictions, which can, in turn, affect estimates of forest productivity. Therefore, it is important to consider site variations based on physiographic factors when predicting MAI [25].
In many countries, especially in South Africa, Tanzania, the DRC, and Zimbabwe, the productivity of forest plantation estates is generally summarized within large compartments/site classes [26]. However, forest productivity estimates downscaled from larger spatial scales can give false expectations of wood supply at the local scale and prevent reasonable estimates of sustainable yields [25]. In many underdeveloped countries, the forest productivity estimates within site class are poorly developed and rarely used in practice. This may partly be due to changes within the site that can only be detected in the longer term [27]. Such changes can be caused, in part, by off-site anthropogenic factors such as the atmospheric deposition of nutrients, site degradation, or climatic change [28,29]. The physiography that characterizes mountainous terrain strongly influences local climate [30], soil characteristics [31], and disturbance regimes [32,33]. Despite the importance of forest productivity in developing countries, there have been few undertakings to capture fine-scale variations in forest productivity within typical management compartments in forest plantations in African countries. Variations in the accuracy of the site index for large compartments/site classes also affect local wood markets and sales of timber since these rely on volume predictions based on the site index.
Forest productivity potential often varies with site index [34]. The site index is defined as the average height of the dominant (Hdom) trees in a forest stand at a given reference age and is one of the most commonly used indicators of site productivity of even-aged stands [35]. This is a more consistent way of assessing site production potential than maximum MAI since Hdom is less affected by planting density and thinning [34]. Site index is influenced by spatial scale variations in environmental factors and their impact on tree growth [35]. Understanding how site-specific factors affect variations in productivity and Hdom in forest plantations is an essential prerequisite for attaining sustainable forest management and patterns of resource use [24]. Still, little knowledge is currently available in many African countries. Potentially, physiographic factors, including elevation, slope, slope positions, and site specificity, play a crucial role in determining variations in MAI and site index, which can lead to shifting or changing site classes within forest plantations [26]. Understanding how these factors affect forest productivity and the site index at smaller spatial scales than predicted using the practiced classification is crucial for effective forest management and sustainable practices.
We therefore studied variations in forest productivity and the site index in P. patula stands in two forest plantations located in different regions of Tanzania and aimed to assess the applicability and generality of the present site classification system. Specifically, we tested the following:
(i)
Whether forest productivity and stand variables are consistent with the assigned site classes within plantations.
(ii)
To what extent Hdom, as predicted by the assigned site classes, is consistent with the realized Hdom within and between plantations and whether the differences in Hdom are related to physiographic factors.
(iii)
How physiographic factors represented by slope and elevation affect forest productivity (MAI) within management compartments, each categorized by a single site class.

2. Materials and Methods

2.1. Study Site Descriptions

This study was conducted within the Sao Hill and Shume forest plantations. Sao Hill forest plantation (SHFP) is situated in the Iringa Region in the southwest of Tanzania, between a latitude of 8°18′ and 8° 33′ S and a longitude of 35°6′ and 35°20′ E (Figure 1). The plantation spans an altitudinal range of 1400 to 2000 m above sea level (m.a.s.l.), with an average altitude of 1634 m.a.s.l. It experiences a mean annual rainfall ranging from 750 to 2010 mm between November and April and temperatures ranging from 15 °C to 25 °C per annum [36]. SHFP covers a total area of 135,903 ha, out of which 86,003 ha is used for commercial tree planting and 48,200 ha is reserved for natural forest, river valleys, and future expansion [37]. Pinus patula occupies the largest plantation area (40,000 ha), followed by other pines (P. elliottii, P. caribaea), with 14,070 ha, and the remaining area covered with cypress (Cuppresus lusitanica), Eucalyptus species (Eucalyptus saligna, E. grandis, E. maidenii), acacias (Acacia melanoxylon, Acacia mearnsii), and Grevillea robusta [37,38,39].
Shume forest plantation (SFP) is located in the western part of the Usambara Mountains in the Lushoto district of the Tanga region. This area is positioned at a latitude of 04°33′–04°42′ S and a longitude of 38°15′–38°16′ E, with altitudes varying between 1650 and 2120 m.a.s.l [40]. The region experiences two rainy seasons, from September to November and March to April, with an average annual rainfall spanning from 800 mm to 2000 mm. The temperature range is approximately 16–22 °C, with occasional minor and unreliable rain (Mluwati) occurring in August and September [41]. The total plantation covers about 4863 hectares and is divided into four plantation blocks, namely the Shume West (1906.7 ha), Shume East (1510.51 ha), Shagayu (693.21 ha), and Magamba blocks (752.84 ha). The main species planted include Pinus patula, Pinus radiata, and Cupressus lustanica.

2.2. Sampling Design

We selected the two largest administrative divisions according to production potential, namely SHFP and SFP. Then, based on official management plan records, the original site index model (Equations (1) and (2)) that fits well for P. patula forest plantations in Tanzania, as described by Malimbwi [42], was used to divide the divisions into four compartments representing site classes (I, II, III, and IV), in ascending order of productivity (Figure A1). The site index model is a suitable generalized growth model for explaining height growth at a reference age for P. patula in Tanzania.
Hdom = a × site × (1 − exp(b × Age))c
where Hdom = dominant height (m), a, b, and c are the coefficients to be estimated, and Site = site index, which is the dominant height at a reference age of 15 years.
This resulted in the following equation:
Hdom = 1.564354 × site × (1 − exp(−0.092288 × Age)1.571869
The suitable site indices obtained through the site index curves at reference ages of 12, 15, 15, and 9 were 22.4, 21.8, 16.9, and 7.6 m (site classes I, II, III, and IV), respectively, at SHFP, while at SFP, they were 22.6, 21.8, 16.9, and 7.6 at reference ages of 12, 15, 15, and 13, indicating site classes I, II, III, and IV, respectively (Table A1).
In each site class, we stratified 12 and 6 quadrant plots measuring 20 m × 20 m (400 m2) each, based on the slope position (i.e., summit, mid, and lower slopes) at SHFP and SFP, respectively (Figure 2). A total of 48 plots with 1960 individual trees and 24 plots with 942 individual trees were measured at SHFP and SFP, respectively (Table 1).

2.3. Field Data Collection

In each plot, the diameter at breast height (DBH in centimeters) was measured for all trees. Six trees per plot, including those with the smallest, medium, and largest DBH, had their height measured to estimate the height of the other trees in each site class. Additionally, the dominant height of the five tallest trees per plot was measured (Hdom in meters) at both studied sites [43]. Tree DBH and height were measured using a vernier caliper and a vertex, respectively. We also measured the physiographic factors within each sample plot, including slope (%) and elevation (m.a.s.l) (Figure 2). Slopes were measured at four corners of each plot using a clinometer, and the average values were recorded. Slope positions were identified by observing contour lines, and their elevations were recorded using a global positioning system (Garmin GPSMAP 65 Series). The ages of the plantations were documented based on management records. Specifically, the ages of the plantations at SHFP ranged from 9 to 15 years, while those at SFP ranged from 12 to 15 years.

2.4. Data Analysis

2.4.1. Data Processing

Table 2 displays the calculated forest stand parameters, including tree height (H), basal area (G), tree volume (V), and mean annual increment (MAI). However, for both plantations, the same species-specific models are employed to estimate these attributes because they are tailored to specific forest tree species.
The Mean Dominant Height (Hdom) was estimated using the height of the five tallest trees of good form in each plot, as described by Vatandaşlar et al. [47].
Stand volume (m3/ha) was estimated in a similar way to the basal area per ha, as described by Malimbwi et al. [45]. The mean annual increment (MAI) of a forest stand was typically measured through the cumulative volume production over time as described by Saka [46] and Matthews et al. [47].

2.4.2. ANCOVA, the Generalized Linear Model, and the Linear Mixed-Effects Model

As some of the stands had different ages, we analyzed the differences in forest productivity and stand variables under different site classes using Covariance Analysis (ANCOVA), in which stand age served as a covariate. With all the trees combined in plots for a given site class, the Generalized Linear Model (GLM) was used to examine the effect of each site class on the forest productivity and stand variables. Then, where significant differences were observed, Student–Newman–Keuls (SNK) post hoc tests were used to determine which means were significantly different at p ≤ 0.05 [48,49]. We also examined the variations between the predicted and realized dominant heights (Hdom) based on the slope positions, one of the physiographic factors, using site index curves in the P. patula forest plantation yield table, as described by Malimbwi et al. [44], to observe shifts in the site classes at SHFP and SFP. Moreover, a linear mixed-effect model (LMM) was used to test whether physiographic variables (slope % and elevations) could account for the heterogeneity of MAI within site classes as described in Equation (3). However, slope percentage and elevations were used as the independent variables.
M A I i j = β 0 + β 1 Slope i j + β 2 Elevation i j + γ k + ϵ i j
where MAIij is the response variable for the I (th) observation in the (j) plot.
β0 is the intercept. β1 and β2 are the fixed-effect coefficients for slope and elevation, respectively. γk represents the random effect for the (k)th plot. ϵ ij is the error term.
The model allows us to partition the total variance in MAI into the variance explained by the fixed effects (slope and elevation) and the random plot-level effect. This can help determine how much of the heterogeneity in MAI is accounted for by the physiographic variables versus other unobserved site-level factors. Only significant parameters (p  <  0.05) were retained. All statistical analyses were conducted and tables and figures made using SAS 9.4 (2011, SAS Institute Inc., Cary, NC, USA).

3. Results

3.1. Forest Productivity and Stand Variables for Assigned Site Classes within Sao Hill and Shume Forest Plantations in Tanzania

The ANCOVA results indicated that at SHFP, the forest productivity and stand variables for site classes (SCs) I and III were similar and lower than for SC II, while Hdom was significantly higher in SC II (Figure 3a). For SFP, the results indicated significant variation in forest productivity between site classes, with the forest productivity and stand variables decreasing from SCs I to IV, as expected. Unlike at SHFP, the stand variables at SFP decreased consistently with SC, except for Hdom and BA, which did not differ significantly between SCs I, II, and III (Figure 3b). For each corresponding SC, the stand variables were consistently lower at SHFP than at SFP (Figure 3a,b).

3.2. Dominant Height (Hdom) as Related to Physiographic Factors and the Shift in Site Classes at Sao Hill and Shume Forest Plantations in Tanzania

Hdom exhibited unexpected shifts in both directions contrary to what was predicted from the original site classes at SHFP and SFP, resulting in shifting site classes (Figure 4a,b). Furthermore, SC I displayed variations at SHFP due to physiographic factors (slope positions). Specifically, Hdom at the summit slope position shifted to site class III, while the mid-slope position shifted to site class II (Table A1). The remaining three SCs did not vary with the slope positions. In contrast, SC II at SFP changed to SC III in the mid-slope position, while SC III shifted to SC II at a lower slope (Table A1). Interestingly, SC IV changed to SC III in all slope positions at SFP.

3.3. Effects of Elevations and Slope Percentage on Forest Productivity within Site Classes at Sao Hill and Shume Forest Plantations in Tanzania

The LMM for the entire dataset showed remarkable evidence for the effect of the elevation and slope factors on MAI (Table 3). Notably, MAI exhibited a significant positive correlation with slope and elevation and hence influenced productivity variations within the forest plantations (Table 3, Figure 5 and Figure 6). The effect of slope depended on the elevation-indicated variations in a forest’s mean annual increment, whereby MAI at SHFP decreased with elevation at a slopes between 8 and 17% (Figure 5a,b) and MAI increased as slope and elevation increased (Figure 5c), while at SFP, MAI increased with elevation at a 7.1%–9.0% slope but decreased with elevation at a 9.1 to 11.0% slope (Figure 6a,b).

4. Discussion

This study demonstrated variations in forest productivity and stand variables for the assigned site classes within the Sao Hill and Shume forest plantations. Our results indicate that MAI and other stand variables vary inconsistently within and between the assigned site classes. Specifically, we found that MAI was significantly higher in SC II at SHFP, while it was significantly higher in SC I at SFP (Figure 3a,b). The differences in the stand variables between site classes could be attributed to a combination of factors, such as superior soil quality, including soil fertility and the availability of moisture [50,51,52,53]; management factors; and other environmental factors, such as light availability and microclimate conditions [34]. Fu et al. [54] suggest that soil moisture content, weather conditions, and crop growth stage are also important fine-scaled factors that can predict production variations. Stendahl [55] reported that detailed fine-scaled information at the regional and small scales within forest stands might lead to better use of forest resources and better information about productivity prediction.
By comparing the measured Hdom based on variations in the slope positions as one of the physiographic factors with sigmoid-shaped curves of the original site index (Figure A1), our results indicated that, in most cases, the measured Hdom did not agree with the previously predicted site class from the original site index model, leading to a change in site class (Figure 4a,b). These findings suggest that variations in Hdom within the stands cause changes in site classes and ultimately influence productivity variations [56,57]. The reasons for this include changes in microclimate patterns, such as increased precipitation or temperatures, which are influenced by different altitudinal gradients [58,59,60]. This also contributes to better conditions for the growth of trees in terms of height and other associated growth attributes, resulting in a gap between the expected volume and the realized volume.
The slope positions contribute to the shift in site classes (Table A1), as they create microhabitats with unique microclimates [61] that may cause stand growth variables to vary [62,63,64]. We found that Hdom differed along the slope position, with the mid and lower slopes recording the highest variations. Steep slope areas, probably due to high soil erosion, often have poorer soil nutrients and a lower water supply than gentle slope areas, and the different amounts of resources trees need to grow will affect the productivity of the trees. Rohner et al. [65] reported that tree growth is higher in gentler and lower-slope areas.
Furthermore, studies by Mgoo et al. [66] and Gumadi et al. [67] reported that changes in site classes within forest plantations can be attributed to a range of natural (pest and disease outbreaks) and human-induced factors (e.g., wildfires). Additionally, unfavorable soil properties, including low fertility, acidic pH, low humus content, poor conditions for mycorrhizal associations, high bulk density and poor soil structure, and fluctuating groundwater levels, may lower forest tree variables [68,69,70,71]. Alterations in soil quality due to erosion, nutrient depletion, or contamination can also influence specific tree species’ growth, consequently impacting site class shifts [72]. This argument is supported by other studies that slope affects the soil properties along elevation gradients [21,73].
Physiographic factors represented by slope and elevation played a significant role in determining the variation in the forest productivity of the P. patula plantations (p < 0.05). We found that elevation and slope significantly but inconsistently affect the productivity within site classes (Table 2). Werner and Homeier [74]; Pierick et al. [21]; Fortunel et al. [75]; and Jucker et al. [76] reported similar findings that elevation and slope variation in forests could be strong drivers that affect productivity in several tropical forests. Hemingway and Kimsey [77] found that forest productivity varies with elevation. Micro-environmental heterogeneity influences the microclimate and short-range soil fertility changes, e.g., the soil fertility tends to be higher at lower elevations, hence improved productivity [22,78]. Physiographic factors also affect microhabitat heterogeneity, which limits light availability, space, soil nutrients, and water, among others [79]. Forest productivity is affected by elevation through associated changes in temperature, moisture, light, and soil properties [80,81]. Also, different slopes can provide valuable insights into the biophysical determinants of maximum productivity and the mechanisms controlling yields. The results indicated that a gentle slope below 20% and elevation below 1900 m.a.s.l (Figure 5 and Figure 6) represent the most optimal slope for the growth and development of P. patula. Our findings highlight the importance of linking physiographic factors to variations in forest productivity to enhance decision-making in sustainable forest management.

5. Conclusions

This study provides valuable insights into the variation in forest productivity and dominant height (Hdom) within the site classes of Pinus patula at the Sao Hill and Shume forest plantations in Tanzania. By assessing variations in forest productivity (mean annual increment (MAI)) and Hdom in relation to physiographic factors in the P. patula stands, based on the site index model originally used to classify productivity, the researchers revealed inconsistencies in the present site classification system used in Tanzania. This study shows that physiographic factors, including elevation and slope, significantly contributed to predicting productivity variations within P. patula stands in Tanzania. Therefore, adopting a more comprehensive and accurate site classification system that accounts for these factors can help practitioners and policymakers make informed decisions regarding management practices, eventually contributing to sustainable forest resource utilization. To address the inconsistencies in the current site classification system for Tanzania’s plantations, it is critical to review the models and methodologies that were originally applied to assess site productivity. Hence, there is a need to revise forest management plans by developing specific prescriptions based on the observed variations in the site classes to attain sustainable forest production. The results emphasize the importance of further research for an improved site classification system elsewhere that considers the influence of physiographic and other environmental factors on the variability of forest productivity.

Author Contributions

Data collection, data curation, formal analysis, methodology, writing—original draft, and writing—review and editing, J.M.; conceptualization, data curation, methodology, writing—revision and editing of the main manuscript, U.I. and J.Z.K.; conceptualization, data curation, methodology, writing—review and editing of the manuscript, S.S.M.M. All authors have read and agreed to the published version of the manuscript.

Funding

We gratefully acknowledge that this research was funded by the Swedish International Development Agency (SIDA), Grant Number 13394.

Data Availability Statement

Data will be made available on request.

Acknowledgments

The authors wish to express their sincere gratitude to the Swedish International Development Agency (SIDA) for generously funding the research conducted within the framework of the REFOREST Programme, which is coordinated by the Sokoine University of Agriculture (SUA). The REFOREST Programme’s collaborative efforts and guidance have been integral to the successful implementation of this study. The authors thank the REFOREST Programme Coordinator—Romanus Ishengoma.

Conflicts of Interest

The authors have no competing interests to declare that are relevant to this article’s content.

Appendix A

Figure A1. Site index curves for P. patula in Tanzania.
Figure A1. Site index curves for P. patula in Tanzania.
Forests 15 01247 g0a1
Table A1. Predicted and measured attributes for the site classes at SHFP and SFP.
Table A1. Predicted and measured attributes for the site classes at SHFP and SFP.
SitesPredicted AttributesMeasured Attributes
Original Site ClassAgePredicted HdomRealized HdomSlope PositionsMicro-Site Classes
(Shifted Site Classes)
SHFPSC I1222.415.65SummitIII
19.08MidII
22.98LowerI
SC II1521.822.65SummitII
24.79MidII
22.07LowerII
SC III1516.919.14SummitIII
20.39MidIII
21.90LowerIII
SC IV97.610.08SummitIV
9.68MidIV
9.27LowerIV
SFPSC I1222.622.46SummitI
25.54MidI
25.61LowerI
SC II1521.822.89SummitII
21.13MidIII
25.52LowerII
SC III1516.920.87SummitIII
22.22MidIII
24.78LowerII
SC IV137.616.03SummitIII
16.85MidIII
17.55LowerIII
Note: SC means site class obtained from administrative records.

References

  1. Boscolo, E.; Rametsteiner, E. Chapter 4 in: The State of the World’s Forests 2022. Discussions, Stats, and Author Profiles for This Publication. Available online: https://www.researchgate.net/publication/360386906 (accessed on 5 May 2024).
  2. FAO. Global Forest Resources Assessment, Main Report. FAO Forestry 2010, Paper No. 163; Food and Agricultural Organisation of the United Nations: Rome, Italy, 2010; p. 378. Available online: https://www.fao.org/docrep/013/i1757e/i1757e.pdf (accessed on 22 April 2024).
  3. FAO. Global Forest Resources Assessment 2015. How Are the World’s Forests Changing? 2nd ed.; Food and Agricultural Organisation of the United Nations: Rome, Italy, 2016; p. 56. Available online: http://www.fao.org/3/a-i4793e.pdf (accessed on 9 December 2023).
  4. Fenning, T.M.; Gershenzon, J. Where will the wood come from? Plantation forests and the role of biotechnology. Trends Biotechnol. 2002, 20, 291–296. [Google Scholar] [CrossRef] [PubMed]
  5. Siry, J.; Cubbage, F.; Ahmed, M. Sustainable Forest Management: Global challenges and opportunities. For. Policy Econ. 2005, 7, 551–561. [Google Scholar] [CrossRef]
  6. Payn, T.; Carnus, J.M.; Freer-Smith, P.; Kimberley, M.; Kollert, W.; Liu, S.; Orazio, C.; Rodriguez, L.; Silva, L.N.; Wingfield, M.J. Changes in planted forests and future global implications. For. Ecol. Manag. 2015, 352, 57–67. [Google Scholar] [CrossRef]
  7. Maxwell, S. Forestry Statistics 2022: Chapter 9 International Forestry. Available online: https://www.forestresearch.gov.uk/statistics/ (accessed on 27 December 2023).
  8. Joson, M. Net Zero Could Drive up the Global Demand for Timber, Putting at Risk the World’s Forests. Features 2022. Available online: https://www.investmentmanitor.ai/features/net-zero-drive-up-global-demand-timber-forests/?cf-view (accessed on 7 July 2024).
  9. Peters, G.P.; Andrew, R.M.; Boden, T.; Canadell, J.G.; Ciais, P.; Le Quéré, C.; Marland, G.; Raupach, M.R.; Wilson, C. The challenge to keep global warming below 2 °C. Nat. Clim. Chang. 2012, 3, 4–6. [Google Scholar] [CrossRef]
  10. Tadesse, W.; Fonseca, T.F. Pinus patula plantations in Africa: An Overview of Its Silvicultural Traits and Use under SDG. In Conifers—Recent Advances; IntechOpen: London, UK, 2022. [Google Scholar] [CrossRef]
  11. Santiago-García, W.; Pérez-López, E.; Quiñonez-Barraza, G.; Rodríguez-Ortiz, G.; Santiago-García, E.; Ruiz-Aquino, F.; Tamarit-Urias, J.C. A dynamic system of growth and yield equations for Pinus patula. Forests 2017, 8, 465. [Google Scholar] [CrossRef]
  12. Kamala, F.D.; Sakagami, H.; Oda, K.; Matsumura, J. Wood density and growth ring structure of Pinus patula planted in Malawi, Africa. IAWA 2013, 34, 61–70. [Google Scholar] [CrossRef]
  13. Ugalde, L.; Pérez, O. Mean Annual Volume Increment of Selected Industrial Forest Plantation Species. In Forest Plantations Thematic Papers; Mead, D.J., Ed.; Food and Agriculture Organization: Rome, Italy, 2001; p. 27. Available online: https://www.researchgate.net/publication/235704736 (accessed on 7 February 2024).
  14. Ndlovu, N.; Little, K.; Titshall, L.; Rolando, C.A. Site preparation and vegetation management impacts on Pinus patula growth and rotation end productivity in South Africa. Aust. For. 2019, 82, 107–115. [Google Scholar] [CrossRef]
  15. Baribault, T.W.; Kobe, R.K.; Finley, A.O. Tropical tree growth is correlated with soil phosphorus, potassium, and calcium, though not for legumes. Ecol. Monogr. 2012, 82, 189–203. Available online: https://www.jstor.org/stable/41739364 (accessed on 17 March 2024). [CrossRef]
  16. Antón-Fernández, C.; Mola-Yudego, B.; Dalsgaard, L.; Astrup, R. Climate-sensitive site index models for Norway. Can. J. For. Res. 2016, 46, 794–803. [Google Scholar] [CrossRef]
  17. Fiandino, S.; Plevich, J.; Tarico, J.; Utello, M.; Demaestri, M.; Gyenge, J. Modeling forest site productivity using climate data and topographic imagery in Pinus elliottii plantations of central Argentina. Ann. For. Sci. 2020, 77, 1–9. [Google Scholar] [CrossRef]
  18. Tymi’nska-Czabańska, L.; Socha, J.; Hawryło, P.; Bałazy, R.; Ciesielski, M.; Grabska-Szwagrzyk, E.; Netzel, P. Weather-sensitive height growth modelling of Norway spruce using repeated airborne laser scanning data. Agric. For. Meteorol. 2021, 308–309, 108568. [Google Scholar] [CrossRef]
  19. Heydari, M.; Mahdavi, A. Relationship between aspect, slope and altitude (physiographic factors), the diversity of plant species (including different case studies in the region, Ilam). In Proceedings of the 3rd National Conference of the Forest, Dehradun, India, 9–11 November 2009. [Google Scholar]
  20. De Castilho, C.V.; Magnusson, W.E.; de Araújo, R.N.O.; Luizão, R.C.C.; Luizão, F.J.; Lima, A.P.; Higuchi, N. Variation in aboveground tree live biomass in a central Amazonian Forest: Effects of soil and topography. For. Ecol. Manag. 2006, 234, 85–96. [Google Scholar] [CrossRef]
  21. Pierick, K.; Leuschner, C.; Homeier, J. Topography as a factor driving small-scale variation in tree fine root traits and root functional diversity in a species-rich tropical montane forest. New Phytol. 2020, 230, 129–138. [Google Scholar] [CrossRef] [PubMed]
  22. Rodrigues, A.C.; Cristina, A.; Villa, P.M.; Ferreira-Júnior, W.G.; Ernesto, C.; Schaefer, R.G.; Neri, A.V. Effects of topographic variability and forest attributes on fine-scale soil fertility in late-secondary succession of Atlantic Forest. Ecol. Process. 2021, 10, 62. [Google Scholar] [CrossRef]
  23. Körner, C. The use of ‘altitude’ in ecological research. Trends Ecol. Evol. 2007, 22, 569–574. [Google Scholar] [CrossRef] [PubMed]
  24. Dessalegn, D.; Beyene, S.; Walley, F.; Gala, T. Effects of topography and land use on soil characteristics along the toposequence of Ele watershed in Southern Ethiopia. Catena 2014, 115, 47–54. [Google Scholar] [CrossRef]
  25. Skovsgaard, J.; Vanclay, J.K. Forest site productivity: A review of spatial and temporal variability in natural site conditions. Forestry 2013, 86, 305–315. [Google Scholar] [CrossRef]
  26. Quichimbo, P.; Jiménez, L.; Veintimilla, D.; Tischer, A.; Günter, S.; Mosandl, R.; Hamer, U. Forest Site Classification in the Southern Andean Region of Ecuador: A Case Study of Pine Plantations to Collect a Base of Soil Attributes. Forests 2017, 8, 473. [Google Scholar] [CrossRef]
  27. O’Hehir, J.F.; Nambiar, E.K.S. Productivity of three successive rotations of P. radiata plantations in South Australia over a century. For. Ecol. Manag. 2010, 259, 1857–1869. [Google Scholar] [CrossRef]
  28. Boisvenue, C.; Running, S.W. Impacts of climate change on natural forest productivity—Evidence since the middle of the 20th century. Glob. Change Biol. 2006, 12, 862–882. [Google Scholar] [CrossRef]
  29. Messaoud, Y.; Chen, H.Y. The influence of recent climate change on tree height growth differs with species and spatial environment. PLoS ONE 2011, 6, e14691. [Google Scholar] [CrossRef] [PubMed]
  30. Daly, C.; Conklin, D.R.; Unsworth, M.H. Local atmospheric decoupling in complex topography alters climate change impacts. Int. J. Climatol. 2010, 30, 1857–1864. [Google Scholar] [CrossRef]
  31. Griffiths, R.P.; Madritch, M.D.; Swanson, A.K. The effects of topography on forest soil characteristics in the Oregon Cascade Mountains (USA): Implications for the effects of climate change on soil properties. For. Ecol. Manag. 2009, 257, 1–7. [Google Scholar] [CrossRef]
  32. Heyerdahl, E.K.; Brubaker, L.B.; Agee, J.K. Spatial controls of historical fire regimes: A multiscale example from the interior west, USA. Ecology 2001, 82, 660–678. [Google Scholar] [CrossRef]
  33. Taylor, A.H.; Skinner, C.N. Spatial patterns and controls on historical fire regimes and forest structure in the Klamath Mountains. Ecol. Appl. 2003, 13, 704–719. Available online: https://www.jstor.org/stable/4134688 (accessed on 15 April 2024). [CrossRef]
  34. Skovsgaard, J.P.; Vanclay, J.K. Forest site productivity: A review of the evolution of dendrometric concepts for even-aged stands. For. Int. J. For. Res. 2008, 81, 13–31. [Google Scholar] [CrossRef]
  35. Weiskittel, A.R.; Crookston, N.L.; Radtke, P.J. Linking climate, growth primary productivity, and site index across forests of the western United States. Can. J. For. Res. 2011, 41, 1710–1721. [Google Scholar] [CrossRef]
  36. Kędziora, W.; Tomusiak, R.; Boreck, T. Site index research: A literature review. For. Res. Pap. 2020, 81, 91–98. [Google Scholar] [CrossRef]
  37. MNRT. Management Plan 2018–2023 for Sao Hill Forest Plantation. 2018; Unpublished work. [Google Scholar]
  38. Ngaga, Y.M. Forest plantations and woodlots in Tanzania. Afr. For. Forum 2011, 16, 1–80. [Google Scholar]
  39. Kangalawe, H. Plantation Forestry in Tanzania: A History of Sao Hill Forests 1939–2015. Ph.D. Dissertation, Stellenbosch University, Stellenbosch, South Africa, 2018. Available online: https://scholar.sun.ac.za/bitstream/handle/10019 (accessed on 8 March 2024).
  40. Lovett, J.C. Elevational and latitudinal changes in tree associations and diversity in the Eastern Arc Mountains of Tanzania. J. Trop. Ecol. 1996, 12, 629–650. Available online: https://www.jstor.org/stable/2559966 (accessed on 23 November 2023). [CrossRef]
  41. Haruyama, S.; Toko, A. Local forest management in Tanzania: A case study from Lushoto District, Usambara Mountain. Soc. Nat. 2005, 1, 586–603. [Google Scholar] [CrossRef]
  42. Malimbwi, R.E. Yield tables for seven Tanzania Forest Service Agency (TFS) forest plantations in Tanzania. Tanzan. J. For. Nat. Consrvation 2016, 90, 3. [Google Scholar]
  43. Zhang, Z.; Wang, T.; Skidmore, A.K.; Cao, F.; She, F.; Cao, L. An improved area-based approach for estimating plot-level tree DBH from airborne LiDAR data. For. Ecosyst. 2023, 10, 1–10. [Google Scholar] [CrossRef]
  44. Mugasha, W.A.; Zahabu, E.; Maguta, M.P.; Mshana, J.S.; Katani, J.Z.; Chamshama, S.A.O. Allometric biomass models for Pinus patula plantations. In Allometric Tree Biomass and Volume Models in Tanzania; Malimbwi, R.E., Eid, T., Chamshama, S.A.O., Eds.; Department of Forest Mensuration and Management, Sokoine University of Agriculture: Morogoro, Tanzania, 2016; pp. 77–84. [Google Scholar] [CrossRef]
  45. Malimbwi, R.E.; Mugasha, W.A.; Mauya, E.W. Development of Yield Tables for Seven Tanzania Forest Service Agency Forest Plantations in Tanzania. Consultancy Report. Tanzania Forest Agency. 2016. 39p. Available online: https://redd.unfccc.int/media/frel__for__tanzania_december2016_27122016.pdf (accessed on 19 November 2023).
  46. Saka, M.G. Determination of mean annual increment and optimal rotation age for sustainable management of Eucalyptus species in Afaka forest reserve, Nigeria. Int. J. For. Ecol. Environ. 2021, 5, 187–194. Available online: https://www.journalbinet.com/ijfee-journal.html (accessed on 22 January 2024).
  47. Vatandaşlar, C.; Seki, M.; Zeybek, M. Assessing the potential of mobile laser scanning for stand-level forest inventories in near-natural forests. For. Int. J. For. Res. 2023, 96, 448–464. [Google Scholar] [CrossRef]
  48. Newman, D. The distribution of range in samples from a normal population, expressed in terms of an independent estimate of standard deviation. Biometrika 1939, 31, 20–30. [Google Scholar] [CrossRef]
  49. Bates, D.; Machler, M.; Bolker, B.; Walker, S. Fitting linear mixed-effects models using lme4. Stat. Softw. 2014, 67, 1–48. [Google Scholar] [CrossRef]
  50. Faraway, J.J. Extending the Linear Model with R: Generalized Linear, Mixed Effects, and Nonparametric Regression Models, 2nd ed.; Taylor & Francis Group: New York, NY, USA, 2016. [Google Scholar] [CrossRef]
  51. Pretzsch, H.; Bielak, K.; Block, J.; Bruchwald, A.; Dieler, J.; Ehrhart, H.-P.; Zingg, A. Productivity of mixed versus pure stands of oak (Quercus petraea (Matt.) Liebl. and Quercus robur L.) and European beech (Fagus sylvatica L.) along an ecological gradient. Eur. J. For. Res. 2013, 132, 263–280. [Google Scholar] [CrossRef]
  52. Toïgo, M.; Vallet, P.; Perot, T.; Bontemps, J.-D.; Piedallu, C.; Courbaud, B.; Canham, C. Overyielding in mixed forests decreases with site productivity. J. Ecol. 2015, 103, 502–512. [Google Scholar] [CrossRef]
  53. Forrester, D.I.; Bauhus, J. A review of processes behind diversity–productivity relationships in forests. Curr. For. Rep. 2016, 2, 45–61. [Google Scholar] [CrossRef]
  54. Fu, R.; Xie, L.; Liu, T.; Zheng, B.; Zhang, Y.; Hu, S. A soil moisture prediction model, based on depth and water balance equation: A case study of the Xilingol League Grassland. Int. J. Environ. Res. Public Health 2023, 20, 1374. [Google Scholar] [CrossRef]
  55. Stendahl, J. Spatial Aspects of Forest and Forest Soil Management. Ph.D. Thesis, Swedish University of Agricultural Sciences, Uppsala, Sweden, 2001. [Google Scholar]
  56. Waring, R.H.; Milner, K.S.; Jolly, W.M.; Phillips, L.; McWethy, D. Assessment of site index and forest growth capacity across the Pacific and Inland Northwest U.S.A. with a MODIS satellite-derived vegetation index. For. Ecol. Manag. 2006, 228, 285–291. [Google Scholar] [CrossRef]
  57. Wang, D.; Hsieh, H.; Tang, S.C.; Chung, C.H. Site index curve for Taiwania plantations in the liukuei area. Taiwan J. For. Sci. 2008, 23, 335–349. [Google Scholar]
  58. Chen, J.; Saunders, S.C.; Crow, T.R.; Naiman, R.J.; Kimberley, D.; Brosofske, K.D.; Mroz, G.D.; Brian, L.; Brookshire, B.L.; Jerry, F.; et al. Microclimate in Forest Ecosystem and Landscape Ecology-Variations in local climate can be used to monitor and compare the effects of different management regimes. BioScience 1999, 49, 288–297. [Google Scholar] [CrossRef]
  59. Muscarella, R.; Kolyaie, S.; Douglas, C.; Morton, S.C.; Jess, K.; Zimmerman, J.K.; Uriarte, M.U. Effects of topography on tropical forest structure depend on climate context. J. Ecol. 2020, 108, 145–159. [Google Scholar] [CrossRef]
  60. Singh, P.; Negi, G.C.S. Microclimate variability under forest canopies along an altitudinal gradient in Western Himalaya. Environ. Anal. Ecol. Stud. 2023, 11, 000765. [Google Scholar] [CrossRef]
  61. Lenoir, J.; Graae, B.J.; Aarrestad, P.A.; Alsos, I.G.; Armbruster, W.S.; Austrheim, G.; Bergendorff, C.; Birks, H.J.B.; Brathen, K.A.; Brunet, J.; et al. Local temperatures inferred from plant communities suggest strong spatial buffering of climate warming across Northern Europe. Glob. Chang. Biol. 2013, 19, 1470–1481. [Google Scholar] [CrossRef]
  62. Burnett, M.R.; August, P.V.; Brown, J.H.; Killingbeck, K.T. The influence of geomorphological heterogeneity on biodiversity I. A patch-scale perspective. Conserv. Biol. 1998, 12, 363–370. [Google Scholar] [CrossRef]
  63. Deák, B.; Valkó, O.; Tóth, C.A.; Botos, Á.; Novák, T.J. Legacies of past land use challenge grassland recovery—An example from dry grasslands on ancient burial mounds. Nat. Conserv. 2020, 39, 113–132. [Google Scholar] [CrossRef]
  64. Deák, B.; Báthori, F.; Lőrinczi, G.; Végvári, Z.; Nagy, D.D.; Mizser, S.; Torma, A.; Valkó, O.; Tóthmérész, B. Functional composition of ant assemblages in habitat islands is driven by habitat factors and landscape composition. Sci. Rep. 2021, 11, e20962. [Google Scholar] [CrossRef]
  65. Rohner, B.; Bugmann, H.; Bigler, C. Estimating the age-diameter relationship between oakspeciesin Switzerland using nonlinear mixed-effects models. Eur. J. For. Res. 2013, 132, 751–764. [Google Scholar] [CrossRef]
  66. Mgoo, O.S.; Mwambusi, J.N.; Chamashama, S.A.O. Effects of thinning regimes on growth and yield of Tectona grandis at Longuza forest plantation, Muheza District, Tanzania. Tanz. J. For. Nat. Conserv. 2022, 91, 1–26. Available online: https://www.researchgate.net/publication/36466160 (accessed on 27 March 2024).
  67. Gumadi, J.; Mwambusi, J.N.; Chamshama, S.A.O.; Andrew, S.M.; Malimbwi, R.E. Thinning compliance and its effects on growth, yield and stem quality of Tectona grandis at Mtibwa forest plantation, Morogoro, Tanzania. Tanz. J. For. Nat. Conserv. 2023, 92, 82–95. [Google Scholar]
  68. Burger, J.A. Soil and its relationship to forest productivity and health. Encycl. For. Sci. 2004, 3, 1189–1195. [Google Scholar]
  69. Morris, L.A. Soil organic matter forms and functions. Encycl. For. Sci. 2004, 3, 1201–1207. [Google Scholar] [CrossRef]
  70. Torreano, S. Soil development and properties. In Encyclopedia of Forest Sciences; Evans, J., Burley, J., Youngquist, J.A., Eds.; Elsevier: Oxford, UK, 2004; pp. 1208–1216. [Google Scholar]
  71. Weiler, M.; McDonnell, J. Virtual experiments: A new approach for improving process conceptualization in Hillslope hydrology. J. Hydrol. 2004, 285, 3–18. [Google Scholar] [CrossRef]
  72. Šamonil, P.; Jaroš, J.; Daněk, P.; Tikhomirov, D.; Novotný, V.; Weiblen, G.; Christl, M.; Egli, M. Soil erosion affected by trees in a tropical primary rain forest, Papua New Guinea. Geomorphology 2023, 425, 108589. [Google Scholar] [CrossRef]
  73. Rezaei, H.; Jafarzadeh, A.A.; Alijanpour, A.; Shahbazi, F.; Kamran, K.V. Effect of slope position on soil properties and types along an elevation gradient of Arasbaran forest, Iran. Int. J. Adv. Sci. Eng. Inf. Technol. 2015, 5, 449–456. [Google Scholar] [CrossRef]
  74. Werner, F.A.; Homeier, J. Is tropical montane forest heterogeneity promoted by a resource-driven feedback cycle? Evidence from nutrient relations, herbivory and litter decomposition along a topographical gradient. Funct. Ecol. 2015, 29, 430–440. [Google Scholar] [CrossRef]
  75. Fortunel, C.; Lasky, J.R.; Uriarte, M.; Valencia, R.; Wright, S.J.; Garwood, N.C.; Kraft, N.J. Topography and neighborhood crowding can interact to shape species growth and distribution in a diverse Amazonian forest. Ecology 2018, 99, 2272–2283. [Google Scholar] [CrossRef] [PubMed]
  76. Jucker, T.; Bongalov, B.; Burslem, D.F.R.P.; Nilus, R.; Dalponte, M.; Lewism, S.L.; Phillips, O.L.; Qie, L.; Coomes, D.A. Topography shapes the structure, composition and function of tropical forest landscapes. Ecol. Lett. 2018, 21, 989–1000. [Google Scholar] [CrossRef] [PubMed]
  77. Hemingway, H.; Kimsey, M. Estimating forest productivity using site characteristics, multipoint measures, and a nonparametric approach. For. Sci. 2020, 66, 645–652. [Google Scholar] [CrossRef]
  78. Yue, Q.; Hao, M.; Li, X.; Zhang, C.; von Gadow, K.; Zhao, X. Assessing biotic and abiotic effects on forest productivity in three temperate forests. Ecol. Evol. 2020, 10, 7887–7900. [Google Scholar] [CrossRef] [PubMed]
  79. Martin-Benito, D.; Cherubini, P.; Rio, M.; Canellas, I. Growth response to climate and drought in Pinus nigra Arn. trees of different crown classes. Trees 2008, 22, 363–373. [Google Scholar] [CrossRef]
  80. Nepal, S.; Mohan, K.C.; Pudasaini, N.; Adhikari, H. Divergent Effects of Topography on Soil Properties and Above-Ground Biomass in Nepal’s Mid-Hill Forests. Resources 2023, 12, 136. [Google Scholar] [CrossRef]
  81. Gairola, S.; Sharma, C.M.; Ghildiyal, S.K.; Suyal, S. Chemical Properties of Soils in Relation to Forest Composition in Moist Temperate Valley Slopes of Garhwal Himalaya, India. Environmentalist 2012, 32, 512–523. [Google Scholar] [CrossRef]
Figure 1. Location of study sites at Sao Hill and Shume forest plantations in Tanzania.
Figure 1. Location of study sites at Sao Hill and Shume forest plantations in Tanzania.
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Figure 2. The location of sampling plots and elevations at Sao Hill and Shume forest plantations in Tanzania. Shaded dots in gray represent studied plots. Rectangles shaded green, pale green, yellow, orange, and red represent elevation range. The different intervals of elevation are influenced by different geographical locations of the plantations.
Figure 2. The location of sampling plots and elevations at Sao Hill and Shume forest plantations in Tanzania. Shaded dots in gray represent studied plots. Rectangles shaded green, pale green, yellow, orange, and red represent elevation range. The different intervals of elevation are influenced by different geographical locations of the plantations.
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Figure 3. Variability in forest productivity estimates and other stand variables as indicated by letter a, b and c with respect to site classes at Sao Hill (SHFP) and Shume forest plantations (SFP) in Tanzania. The vertical line outside the box represents the minimum and maximum values. Means denoted with the same letter are not significantly different (α = 0.05). SC I = site class I; SC II = site class II; SC III = site class III; SC IV = site class IV.
Figure 3. Variability in forest productivity estimates and other stand variables as indicated by letter a, b and c with respect to site classes at Sao Hill (SHFP) and Shume forest plantations (SFP) in Tanzania. The vertical line outside the box represents the minimum and maximum values. Means denoted with the same letter are not significantly different (α = 0.05). SC I = site class I; SC II = site class II; SC III = site class III; SC IV = site class IV.
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Figure 4. Shift in site classes at Sao Hill forest plantation (SHFP) and Shume forest plantation (SFP) in Tanzania: the difference between the predicted and realized Hdom allows for site class shifts at SHFP and SFP compared to those reflected in the original site index model. The color indicates site classes. SCI = site class I; SCII = site class II; SCIII = site class III; SC1V = site class IV. The site class I at SHFP been distributed to SC II and SCIII while at SFP there is an interchange in SCII and SCIII but SCIV been completely shifted to SCIII.
Figure 4. Shift in site classes at Sao Hill forest plantation (SHFP) and Shume forest plantation (SFP) in Tanzania: the difference between the predicted and realized Hdom allows for site class shifts at SHFP and SFP compared to those reflected in the original site index model. The color indicates site classes. SCI = site class I; SCII = site class II; SCIII = site class III; SC1V = site class IV. The site class I at SHFP been distributed to SC II and SCIII while at SFP there is an interchange in SCII and SCIII but SCIV been completely shifted to SCIII.
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Figure 5. Mean predicted variations in response variable over the different observed ranges of slope percentages and elevation interactions in Sao Hill forest plantation (SHFP) in Tanzania. The blue area around the fitted line shows the confidence region. (a,b) MAI decreased with elevation at a slopes between 8 and 17% while (c), MAI increased as slope and elevation increased (c).
Figure 5. Mean predicted variations in response variable over the different observed ranges of slope percentages and elevation interactions in Sao Hill forest plantation (SHFP) in Tanzania. The blue area around the fitted line shows the confidence region. (a,b) MAI decreased with elevation at a slopes between 8 and 17% while (c), MAI increased as slope and elevation increased (c).
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Figure 6. Mean predicted variations in response variable over the different observed ranges of slope percentages and elevation interactions in Shume forest plantation (SFP) in Tanzania. The blue area around the fitted line shows the confidence region. (a) indicates that MAI increased with elevation at a 7.1%–9.0% slope while (b), MAI decreased with elevation at a 9.1 to 11.0% slope.
Figure 6. Mean predicted variations in response variable over the different observed ranges of slope percentages and elevation interactions in Shume forest plantation (SFP) in Tanzania. The blue area around the fitted line shows the confidence region. (a) indicates that MAI increased with elevation at a 7.1%–9.0% slope while (b), MAI decreased with elevation at a 9.1 to 11.0% slope.
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Table 1. Number of plots used for tree growth variable data collection.
Table 1. Number of plots used for tree growth variable data collection.
Forest PlantationsCompartmentsSite ClassesAge (Years)PlotsNo. Trees
SHFPITIMBO 1I1212462
ITIMBO 2II1512539
ITIMBO 3III1512556
ITIMBO 4IV912403
Total 481960
SFPSHUME WEST 45, SHUME EAST 189I126233
SHUME WEST 35, SHUME EAST 187II156226
SHUME WEST 43A, SHUME EAST 164III156255
SHUME WEST 67, 181AIV136228
Total 24942
Table 2. Studied forest stand parameters for Sao Hill and Shume forest plantations in Tanzania.
Table 2. Studied forest stand parameters for Sao Hill and Shume forest plantations in Tanzania.
ParametersModelReference
Tree total height h e i g h t = 1.3 + d b h 2 13.63898 + 0.026482 × d b h 2 Mugasha et al. [44]
Basal areaG = 1⁄m ∑ (gi/ai)Malimbwi et al. [45]
Single tree volumeV = exp(−9.04925 + 1.14781 × ln (Ht) + 1.5496 × lnDbhMalimbwi et al. [45]
Mean annual increment (MAI) M A I a = Y a a Saka [46]
Note: Tree total height = estimated total tree height (m); dbh = measured diameter at breast height (cm); G = basal area per ha; (m2/ha); gi = tree cross-sectional area (gi = π × Dbh2/4); m = number of sample plots; ai = plot area; MAI = mean annual increment (m3 ha−1 yr−1); Ya is yield at age a and a is the age.
Table 3. Results of LMM in estimating the variation in MAI as a dependent variable with elevation and slope as predictive variables at Sao Hill forest plantation (SHFP) and Shume forest plantation (SFP) in Tanzania.
Table 3. Results of LMM in estimating the variation in MAI as a dependent variable with elevation and slope as predictive variables at Sao Hill forest plantation (SHFP) and Shume forest plantation (SFP) in Tanzania.
SitesParameterEstimateStandard Errort-Valuep-Value
SHFPIntercept−24.0665.375−4.4770.024
Slope%1.6870.4863.4720.016
Elevation0.0130.0034.4960.024
Slope% × Elevation−93.272.638 × 10−4−3.3850.018
SFPIntercept−40.1598.5192.74<0.001
Slope%4.4830.92790.904<0.001
Elevation0.0220.005115.685<0.001
Slope% × Elevation−0.0025.107 × 10−490.074<0.001
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Maguzu, J.; Ilstedt, U.; Katani, J.Z.; Maliondo, S.S.M. Variations in the Forest Productivity of Pinus patula Plantations in Tanzania: The Need for an Improved Site Classification System. Forests 2024, 15, 1247. https://doi.org/10.3390/f15071247

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Maguzu J, Ilstedt U, Katani JZ, Maliondo SSM. Variations in the Forest Productivity of Pinus patula Plantations in Tanzania: The Need for an Improved Site Classification System. Forests. 2024; 15(7):1247. https://doi.org/10.3390/f15071247

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Maguzu, Joshua, Ulrik Ilstedt, Josiah Zephaniah Katani, and Salim S. M. Maliondo. 2024. "Variations in the Forest Productivity of Pinus patula Plantations in Tanzania: The Need for an Improved Site Classification System" Forests 15, no. 7: 1247. https://doi.org/10.3390/f15071247

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