Article info

Volume         9   

Pages             42-58

DOI                10.5027/jnrd.v9i0.05

Published     20/08/2019

Keywords    Carbon stock, Corrugated iron sheet cover, Grass cover, Houses, Landuses, Trees

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Author

Miftah Fekadu *ab, Tsegaye Bekele a, Sisay Feleke c

a Hawassa University, WGCFNR, P.O. Box: 128 Shashemene, Ethiopia

b Central Ethiopia Environment and Forest Research Center, P.O. Box: 30708, Addis Ababa, Ethiopia

c Wood Technology Research Center, P.O. Box: 2322, Addis Ababa, Ethiopia

 

* Corresponding author: mfkedir@gmail.com

 

Abstract

In Ethiopia, wood was the main construction material for rural houses. In 2013, about 79% of the rural houses of Ethiopia were fully made of wood. Although carbon storage of wood is well known for climate change mitigation, there is lack of information on carbon stock of wooden houses in Ethiopia. Thus, a study was conducted to analyze the carbon stock of dominant land uses that surround rural wooden houses in three agro-ecologies and representative three peasant associations (PA) or Kebeles in Southern Ethiopia. Field measurement and household survey were made by selecting sixty-four houses made of wood, grass or corrugated iron sheet. Transects were laid starting from the wooden houses to lay out plots to collect samples of wood, grass, soot inside houses, soil and trees for carbon determination. The service age of wooden houses was estimated in triangulated interview as 5-150 years. The total carbon stock of newly constructed rural grass covered wooden house was 28.35- 49.26 kg C m-2, which was greater than the other surrounding land uses. The grazing land total carbon stock was 50.5-86.8% and the scattered trees carbon was 9.5-59.7% of the total carbon stock of the respective PA grass covered wooden house. Since soil is the common below ground carbon stock, the total carbon of a land use is mostly affected by the above ground carbon stock. Grass covered houses contained greater above ground carbon stock but grazinglands contained greater below ground carbon stock. Soot accumulation of 0.4-1.3 g m-2 inside the houses’ roof indicated the presence of indoor pollution. The total carbon stock increased with increasing altitude and geoclimatic variables were significantly correlated with carbon stock of the land uses (p<0.05; r = ±0.999). Therefore, wooden houses need to be considered in climate change mitigations. The shift of carbon stock from natural environment to wooden houses in human dominated landscapes was indicator of a lack of forests, and then efforts should be strengthened to increase forest cover.

 

1. Introduction

Carbon storage in terrestrial carbon sinks like trees, harvested wood products and soils for longer periods of time mitigates climate change (Sheikh & Pandit, 2014). In the carbon cycles (IPCC, 2014), soils are the major stores of carbon in terrestrial ecosystems depending on climate, soil bulk density, and soil depth (Laganière, Angers, & Paré, 2010; Li, Niu, & Luo, 2012). Forests store about 86% of the terrestrial aboveground carbon and 73% of the earth’s soil carbon (Yin et al., 2012). Presence of forests also affect soil carbon (Chang et al., 2011; Deng et al., 2013; IPCC, 2014; Lange et al., 2015; Li, Niu, & Luo, 2012) and other environmental carbon pools in living and dead biomass (IPCC, 2006; Iticha, 2017; Vashum & Jayakumar, 2012). Plant biomass organic carbon vary among the branch, stem and roots of a species, growth stage, topography and site characteristics (Chen et al., 2015; Martin, Doraisami, & Thomas, 2018; Shankar et al., 2014; Sileshi, 2014; Zhang, Guan, & Song, 2012). For example, the carbon content of trees in softwood and hardwood usually is in leafy crown 16.8% and 24.4%; debarked log 51.2% and 46.4%; bark 10% and 6%; stump 2% and 3%; and roots 20% each, respectively (Potter & Woodrom, 2017). Changing forest land use into grass land and agricultural ecosystems reduces soil organic carbon stock by 12-30% (Don, Schumacher, & Freibauer, 2010). Global Forest Resources Assessment in 2010 estimated that the world’s forests store more than 650 Gt C. Moreover, the global forests ecosystems including soils store about 4500 Gt CO2 and land use change and forest land degradation are sources of 20% of the global greenhouse gas (GHG) emission (IPCC, 2007).

Rural wooden houses entirely constructed from woody and nonwoody biomass store carbon as coal, charcoal and wood (Zeng et al., 2013). That is promoting long-lived forest products in wood-framed buildings store carbon (Ilyas, 2013). For instance, the carbon density of urban settlement with wood is 23- 42 kg C m-2 (Churkina, Brown, & Keoleian, 2010) which is higher than the 4-25 Kg C m-2 of tropical rain forest (Baccini et al., 2012; Pan et al., 2011). The carbon pools in wooden houses are harvested wood and grass called dead wood and grass, which could be sound, intermediate and rotten biomass (Casarim & Grais, 2013). In Ethiopia, 79.8% of the total population, or over 84.4 million people lived in rural areas in 2017 (UN DESA, 2017) and wood was the main construction material in 2013 fully in 79% of rural houses and with stone incorporation in 21% of the houses (Central Statistical Agency and World Bank, 2013).

The roof of the houses is covered either by grass or corrugated iron sheet, so are called wooden houses. The grass roofed houses have a traditional thatched-grass, conical roof with circular floor and wall, while the corrugated iron sheet covered houses have rectangular floor and wall but triangular and trapezoidal roof (Alemayehu, 2011). Moreover, rural households use biomass for cooking and heating that form soot (IPCC, 2014). This soot carbon stored in rural houses exhibited indoor pollution (Kankaria, Nongkynrih, & Gupta, 2014).

Understanding the variability of carbon in co-occurring and adjoining land uses in rural settings like scatted trees, woodlands, wooden houses and grazing lands would enable to support the process of reducing emission and the sustainable management of natural resources (Svob, Arroyo-Mora, & Kalacska, 2014). In Ethiopia, forest resources stored about 2.76 Gt C in the above ground biomass (Moges, Eshetu, & Nune, 2010) and soils stored about 14 Gt C (Shiferaw, Hurni, & Zeleke, 2013), however, there is lack of information on the carbon content of individual tree species and the carbon stock of rural wooden houses. Accordingly, it is important to understand the dynamics of carbon sinks in and around human dominated landscapes of rural wooden house settlements in order to design strategies that improve the carbon storage (Western Australian Planning Commission, 2013). Therefore, this study was conducted to address the aforementioned problems with the objective to determine the carbon stock of wooden houses in comparison to surrounding scattered trees and grazing land uses by identifying the types of woody plant species that were used for wooden house construction.

 

2. Material and Methods

2.1 Description of the study area

The study was conducted in Southern Ethiopia, Enemorina Ener district’s three peasant associations (PA) now called Kebele (Awed, Daemir and Ener Kola). The three PAs each were representatives of three different agro-ecologies called highland, midland and lowland at 500-1600 m, 1600-2400 m and 2400-3200 m altitude above sea level (asl), respectively (Figure 1). The rural people of the study area had subsistence agriculture, a kind of mixed farming and depend on local vegetation for fuel and construction. Eucalyptus globulus Labill. poles in highland; E. camaldulensis Dehnh. poles in midland; and Cordia africana Lam. lumber and charcoal making in the agro pastoral lowland were the main tree products cash sources. Each PA covers an area over 800 ha, part of which may fall in different agro-ecology at a given altitudinal range, for example in 500-1600 m asl, 1516 m was specifically sampled (Table 1).

The soils of the study area were free of gravel except close to river sides and degraded areas. The highland had rugged topography with ferric sandy loam soils (Table 1). The district was also described by Negussie (2004) and the precipitation and temperature is given in Figure 2.

In 2005-2013, the mean monthly precipitation in Enemorina Ener district, capital town, Gunchire was 21.65-266.5 mm, with annual mean of 1290 mm as indicated in the Ethiopia Meteorological data, but in lowlands 900, midland 1150 and highlands 1400 mm was conventionally known on average (Bekele-Tesema, 2007). The main rainy season is June to September. In 2005-2013, the neighboring district’s maximum monthly temperature was 21.7-26.8 °C and minimum temperature was 6.7-11.9 °C (Figure 2) but in lowlands 24.25, in midland 18.5 and in highlands 13.5 °C was conventionally known on average (Bekele-Tesema, 2007).

Figure 1: Location map of the study area. (The scale of the map refers only to the three peasant associations or Kebeles and their surroundings).

 

2.2 Methods of data collection and analyses

The study area was selected based on discussion at district level by considering the differences in the altitudinal range that affect the agro-ecology and availability of different plant species (Sheikh, Kumar, & Bussmann, 2009). Each PA was selected to represent an agro-ecology. In each PA, stratified random sampling was used to select houses, in two steps. First, houses with common internal and external wood structures, called standard wooden houses that were covered their roof with grass or corrugated iron sheet were assessed and selected. The nonstandard houses built from crop residues like maize stalks and grass were exclude from the study. Secondly, 30% of the standard wooden houses were randomly selected (Bryman, 2012). At the selected PA’s specific altitude 23,35 and 6 houses (Table 1) were selected, interviewed and measured in Awed PA; Daemir PA; and Ener Kola PA, respectively. Totally, 64 households’ heads, both men and women, were selected and convinced to voluntarily participate in the activities after explaining the purpose of the research. The house owners were interviewed about the age of house (month and year of construction), the type of tree species used for each part of the house, the number of wood used for different parts of the house, and the size of the house. Then the interview results were validated by visual observation, counting, triangulated interview of local elders, Kebele officials and house constructors (engineers) who construct the house. The dimensions were measured using graduated poles and measuring tape.

Land uses around the wooden houses were many but carbon stock was determined for three dominant landuses that occupy most of the area and available to all households including grazing land, scattered live trees, or wood lands (scattered trees in patches and plantations) and wooden houses.

2.2.1 Wooden houses and construction wood sampling and analyses

Wooden houses and wood were measured depending on the geometric shape. The circular grass covered houses diameter and the rectangular corrugated iron sheet covered houses perimeter (length and width) were measured at the flat ground (water level) of the houses using measuring tape. The area of grass covered wooden houses was determined using Equation 1 (West, 2015).

Where: A1: area of circular grass covered wooden house (cm2); π is a constant value 3.142 and D is the internal diameter of the circular grass covered house (cm) (Figure 3a ).

The area of corrugated ironsheet covered rural wooden houses (Figure 4) was determined using Equation 2 (West, 2015).

A2 = LW                                                                                                                                            Equation 2

Where: A2: area of corrugated iron sheet covered wooden house (cm2); L is length (cm) and W is width of rectangular house (cm).

The length, diameter, thickness and width of all the dead wood contained in a house, based on shape of wood, was measured using measuring tape and graduated pole. In straight, round wood, diameter at midpoint and total length but in regularly split wood like lumber, length (L), width (W) and thickness (T) at midpoint was measured and its volume was calculated as Equation 3.

V = LWT Equation 3

Where: V: volume of wood (cm3), L is length (cm), W is width (cm) and T is thickness (cm).

In all types of dry or dead wood used for house construction, three replications of representative wood samples were taken to determine full weight using balance (Adam Lab.equipment Leicester LE67FT-England 0.1 g). The volume of round wood, split wood (Figure 5), and lumber like wood (immersed in water for 24 hours) was calculated using Huber formula (Waddell, 1989; West, 2015) and the volume of lumbers added to give the full log volume (Cruz de León & Uranga-Valencia, 2013) (Equation 3 and Equation 4) to get the mass from basic density.

Where: V: volume of log (cm3); π is a constant value 3.142, D is mid diameter (cm) and L is the length of log (cm).

Basic wood density for dry wood and household utensils, called dead wood (Casarim & Grais, 2013), was determined by the ratio of oven dried (105 °C) weight to green volume. Smaller household utensils such as local chair and lumbers for house partitioning were considered as the houses carbon storage structures and the density was determined from a fraction of the lumber used to make the utensils. Then green volume of small samples was determined by water displacement method (immersed in water for 24 hours) (Govett, Mace, & Bowe, 2010; Williamson & Wiemann, 2010) using distilled water and graduated cylinder. The three replications of small samples for basic wood density were straight, undamaged, nonporous, debarked or undebarked, knot-free, 20-25 mm thick and 25 cm long dry wood taken at midpoint of the wood used for construction. In the case of below ground dead wood about 1m of the central axis, and 50 cm of the surrounding wall, three representative samples from each species (dug out, cleaned and immersed in water for 24 hours) were measured for basic density. Any rooten wood part from samples was removed before measurement. The wood samples for basic density were in ranges of 1-150 years old, which were grouped in to five years, 30 samples, sample 1 for 1-5 years, sample 2 for 6-10 years and sample 3 for 11-15 years etc. Carbon stock in the sampled wood was determined using mass or basic density and volume, and carbon concentration of wood (Krajnc, 2015). For over bark measured wood, sample wood carbon with bark was used. The basic density and carbon content of wood were kept constant for a given part of a tree species.

The total weight of grass used in grass covered wooden house was obtained stepwise; first, the number of manloads of grass used per house was interviewed to selected men and women house owners and checked by counting. Manload is a local measurement unit of weight that can be carried by a matured person. Then three to five samples of manload of airdried grass were weighed using weighing balance (Adam Lab.equipment Leicester LE67FT-England, 0.1 g) in each PA study site to get the average weight of a manload of grass. Oven dry weight (105 °C) of each manload was determined from samples, and then the total dry weight of the grass of the house was extrapolated.

2.2.2 Soot of wooden houses sampling and analyses

Soot is an indoor pollutant, black carbon, resulting from incomplete combustion of fuel. Soot was sampled by clearing all the internal parts of roofs (top part) of wooden houses (Figure 3b and Table 2, No 4). Soot samples were collected from 13 houses covered with grass and 6 houses covered with corrugated iron sheet of volunteer households using brooms. The samples were collected every 4 months and weighed using a balance (Adam Lab. Equip. Leicester LE67FT-England, 0.001 g). It was observed as a usual practice that rural households clear the soot from the internal roof of wooden houses during holidays in the study area twice to three times per year.

2.2.3 Grazing land sampling and analyses

In grazing land, grass and soil samples were taken in three representative pits and plots, respectively; within 1 km three replications of transects from the houses, at 300-400 m distance between transects and plots (Figure 6). The first plot was determined systematically, where grasses exist at 300-400 m distance from the houses.

Soil pit about 1 m x 1 m x 1 m was dug and soil samples were collected at vertical profile of five soil depths 0–5 cm, 5-15 cm, 15-30 cm, 30-50 cm and 50-100 cm. In each soil depth three cores were sampled as a replication for the depth in dry season, March-April 2015.

The soil bulk density (Equation 5) was determined as the ratio of oven dried weight to core volume (5 cm cube) (Equation 6) (Makhuvha, Arellano, & Harney, 2014). Live grass samples were collected at 1 m x 1 m above each soil pit, oven dried (105 °C) and weighed using balance (Adam Lab.equipment Leicester LE67FT-England, 0.001 g).

Where: BD: bulk density of soil (g cm-3); M is mass of oven dried soil sample (g) and V is volume of soil sample corer (cm3).

The volume of soil sample corer was determined by Equation 6.

Where: V: volume of soil sample corer (cm3); D is core diameter (cm) and H is the height of corer (cm).

2.2.4 Scattered, standing live trees sampling and analyses

Scattered, standing live trees sampling was done in the same way as section 2.2.3. The first plot was determined systematically, where woody plants exist at 300-400 m distance from the houses. The standing volume of scattered live trees (UNFCCC, 2001) with height ≥ 2m and diamtere ≥ 5cm was estimated using diameter at breast height (DBH) (1.3 m from the ground surface) and total height measured (Government of Alberta, 2012) using diameter tape and graduated pole, respectively, in 3-5 plots of 5.64 m radius in each PA. Three to 11 trees /shrubs of selected species used for house construction were cut to measure their above ground biomass and stem form factor (Equation 7 and Equation 8), moisture content (Equation 9), carbon content and wood density.

Where: ff: form factor, Vi, n is the volume (cm3) of cut logs from the first log: i = 1 to the last log= n of close to 100 cm length as:

V1 = π(D1)2/4; V2 = π(D2)2/4…; Vn = π(Dn)2/4; D is middiameter of cut logs (cm); Vc is the standing cylindrical volume (cm3) of a tree as:
Vc = π((DBH)2/4) * (H); DBH is diameter at breast height (cm); H is total height (cm).

The volume of standing live trees were determined by Equation 8.

Where: Va: the actual volume (cm3) of standing tree; Vc is the cylindrical volume (cm3) of tree; ff is form factor; ij is the ith species and jth replication; n is replications.

Where: MC: moisture content (%); Wi is initial weight (g); Wf is final weight (g).

The cut trees were divided into different biomass fractions. Branches ≥ 5 cm diameter were added to stem and branches <5 cm diameter considered as twigs and leaves. The weight of the sample wood was measured by digital balance (Adam Lab.equipment Leicester LE67FT- ngland 0.1 g). The below ground root biomass was assumed to be 20% of the above ground. The weight of residues including leaves and barks were considered to be used as biomass energy, proportionally 24.4% and 6% of the total weight of a given tree, respectively (Potter & Woodrom, 2017).

2.2.5 Carbon analysis in laboratory from wood, grass, soot and soil samples

The organic carbon content of plant materials (wood, grass and soot) was determined by repeated measures made using Walkley and Black (1934) procedures by making the weight of the ground dry sample as small as 0.125-0.5 g and 1 mm sieved because of high carbon concentration in plant cells. However, in the presence of a muffle furnace, the cheap and easy procedure of loss on ignition method that uses 5-10 g dry plant material sample at 400 ºC for four hours and with 0.58 factor of ash percent can be used as the carbon (Wang, Wang, & Zhang, 2012). In determining soil organic carbon, about 1-2 g air dried soil sample, <2 mm sieved was used by Walkley and Black (1934) method. Then samples in each plant and soil were prepared separetly in flask and 10 ml, 1N K2Cr2O7 solution was added with pipette to samples (V1) and blank (V2) followed by addition of 20 ml concentrated H2SO4. Then 200 ml distilled water was added to cool. About 10 ml concentrated Orthophosphoric acid was added before titration in the presence of 0.5 ml barium diphenylamine sulphonate indicator. The sample and blank were titrated with 0.5 N ferrous sulfate solution drop by drop until green to light green end point. In this method 77% of the carbon was assumed to be oxidized by potassium dichromate and a correction factor of 100/77 or 1.3 was used (Equation 10).

Where: OC: Organic carbon (%); N is normality of K2Cr2O7 solution (mole eq.-1/ 1000 ml); V1 is volume (ml) of ferrous sulfate solution used for the blank; V2 is volume (ml) of ferrous sulfate solution used for the sample; S is weight (g) of air-dried sample; 0.39 is constant value (0.39= 3 x 10-3 x 100 x 1.3 (3 is equivalent weight of carbon)) (Walkley & Black, 1934); mcf=moisture correction factor as 1+mc%.

The total organic carbon storage of wood in houses was calculated as the sum of the carbon stocks of the different components of tree species wood (Equation 11) and grass (Equation 12) in the case of grass covered houses; and wood only in the case of corrugate iron sheet covered houses.

Where: Cw: Carbon storage of wood (g); BD is basic density of a given part of wood of a species (g cm-3); V is volume of a given part of wood of a given species (cm3); OC is organic carbon content of a given part of a given species (%); ij is the ith species and jth replication; n is the number of replication.

Where: Cg: carbon storage of grass (g); Mgr is mass of grass (g); OC is the organic carbon content of grass (%).

The soil carbon at a given depth in t C ha-1 was calculated as Equation 13.

Where: SOCs: soil organic carbon stock (t C ha−1), d is depth or thickness of the soil (cm), OC is organic carbon (%), BD is bulk density (g cm-3) (Sanderman, Farquharson, & Baldock, 2010).

The Pearsons correlation of landuses carbon with geo-climatic variables and wood density was calculated as Equation 14.

Where: r: correlation coefficient, X is geo-climate: altitude (m); precipitation (mm); temperature (°C) or wood density (g cm-3) and Y is the carbon storage of different land uses (t C ha-1).

 

3. Results

The carbon storage of a landuse depends on the composition of the landuse and its size. The wooden houses carbon stock varied with the type of plant species used for construction because different plant species have different carbon content.

3.1 Major tree species used for house construction

Two types of houses were constructed in the study area using top roof cover of either grass or corrugated iron sheet. As shown in Figure 7, for house construction, different tree species were used in different agro-ecologies. In highland PA, Eucalyptus globulus and Yushania alpina were dominantly used, accounting 69.7 and 18.1 % (w/w) of the wood in grass covered wooden house; and 90.9 and 6.9% of the wood in corrugated iron sheet covered house, respectively. In midland PA, E. camladulensis was dominantly used, accounting 98.5% of the wood in grass covered house and 97.2% of the wood in corrugated iron sheet covered house. In lowland PA, Euclea schimperi and Combretum molle were used, accounting 26.6 and 19.5% of the wood of the grass covered house, respectively (Figure 7). E. camaldulensis and C. africana were used for house construction in all of the agro-ecologies because of availability and quality, respectively. The grass species used were different in different agro-ecologies but generally named as grass. C.africana, J. procera, F. sur and rarely E. camaldulensis lumber (sawn wood) were used for internal partitioning, making doors and windows of both types of houses. There was 14 different parts of a grass covered wooden house including roof covered by grass, central axis and surrounding wall (Figure 3 and Table 2). Corrugated iron sheet covered houses have six major parts including vertical wall, horizontal wall fastener, beam (roof) and pillars (big corner walls); internal partition, doors and windows.

3.2 Shape, and size of wooden houses

The shape of house was mainly determined by the availability of material for construction, economic status and the preferred aesthetic value of the house to the households. Most of the grass covered houses were circular and most of the corrugated ironsheet covered houses were rectangular (Table 3). However, there were very few corrugated ironsheet covered houses and grass covered houses with circular and rectangular shapes, respectively, which were not included in this study. The size of house was determined by the availability of wood and economic capacity of households. The size of grass covered wooden house was 59.0- 78.7 m2 while the corrugated iron sheet covered wooden houses was 78.1 - 110.3 m2, with conical and rectangular floor, respectively (Table 3). Greater size of house was observed in midland because of the availability of wood from Eucalyptus plantion forest (Figure 7). It was also observed that the size of corrugated ironsheet covered houses was greater than grass covered wooden houses (Table 3) because of the improvement in economic status of households.

 

3.3 Carbon storage of scattered trees, wooden houses and grazing land

As observed and responded by the households, the wood used for both grass covered and corrugated ironsheet covered houses was the same type of species that is available in the locality or in the nearby market. As can be seen from Table 4, the density and carbon content of wood, grass and soot used for grass and corrugated iron sheet covered houses at specified moisture content was different. The soot is the byproduct in biomass combustion accumulated in the internal roofs of both types of house covers. The size of wood or diameter at breast height (DBH) used was different for different parts of the house. That is the values in Table 4 are from samples taken from different houses but from the same plant species in a given altitudinal range or peasant association. In the woods of trees used for house construction, the highest carbon concentration of about 59.2% was found in matured stem wood lumber of C. africana and the lowest about 19.9% in young wood of E. camaldulensis (Table 4). Matured tree species like E. globulus grown for 60-80 years have carbon content of 53.7% (Table 4). The overall mean carbon content of the wood used for house construction was 46.7%. The densest wood was obtained at the stump height of Grewia species (0.92 g cm-3), while the lightest from young trees of E. camaldulensis (0.33 g cm-3) (Table 4). The overall mean density of wood used for construction was 0.682 g cm-3. The carbon content of grass was the highest in the highland about 50% and the lowest in lowland about 48% (Table 4). The carbon content of soot was the highest in highland grass covered wooden houses about 50.4% and the lowest in midland corrugated ironsheet covered houses about 32% (Table 4).

The carbon storage time of wood used for grass covered wooden houses was estimated to be 16-100 years in highland, and 5-70 years in lowland PA but for corrugated iron sheet covered houses from 54.2 -150 in highland PA and 34.3-124.1 in midland (Table 5). However, the service life of the whole houses was 20.8-107.1 years (Table 5). The service life was lower than the carbon storage time because all the wood used for construction did not have equal durability. The service life of houses could terminate when most of the wood decompose, but still some durable wood type will remain without decomposition and keep the carbon for longer period of time in the same or different places.

 

In the soil, the carbon content was significantly higher (p< 0.05) at the top 0-5 cm depth than the others depths (Table 6). At 1 m depth the highest mean carbon concentration (17.33 mg C g-1) was obtained in midland and the lowest (10 mg C g-1) in lowland (Table 6).

The above ground carbon storage of grass covered wooden house was 28.4 - 49.21 kg C m-2 when the house construction was completed (Table 7). The grazing land grass and soil carbon stock varied locally and it ranged in lowland to highland from 0.127- 0.185 kg C m-2 and 24.473- 28.213 kg C m-2, respectively (Table 7).

Rural grass covered wooden houses were serving for 15-30 years in Ener Kola, lowland PA and 44-100 years in Daemir, midland PA with mean of 20.8- 69.2 years. The corrugated iron sheet covered wooden houses were serving for 66-125 years in Daemir PA and 90-120 years in Awed PA, with mean of 99-107 years, depending on the durability of wood used (Table 5). The service age of wooden houses is determined by the type of wood, agro-ecology and the presence of decomposing agents. If the wood decomposes easily, converted to CO2 and other components of the wood, the service age will be less. It was observed that Juniperus species using cold climate highland houses have longer age than the others because of the species’ resistance to decomposition. Since the wooden house comprise different species of wood, the carbon storage also depends on the species. The carbon storage was 5.2-100 years in the case of grass covered houses and 34.3-150 in the case of corrugated iron sheet covered houses (Table 5). The 16.8-100 years carbon storage but the 50-80 years service age in Awed, highland PA, forexample, can be attributed to the decomposition of some of the wood used in the house construction but the house may serve in the presence of some of the wood components. Some of the wood could serve additional years in the new construction even after the total collapse of the old house.

Table 7 showed that the total carbon stock of grass covered houses was greater than the other landuses studied. The carbon storage in corrugated iron sheet covered wooden house of highland and midland agro-ecology (357.00*10-4 – 637.00 *10-4kg C m-2) was less than the grass covered wooden house because of the presence of grass in the later (Table 7). There was no corrugated iron sheet covered wooden houses in lowland, Ener Kola PA. The above ground carbon stock of the grass covered wooden house was also greater than the other landuses studied. However, the greatest below ground carbon storage was observed in grazing land soil followed by the scattered trees landuse (Table 7).

 

The grazing land use grass and soil total carbon stock was 50.5-86.8% and the remnant scattered trees carbon was 9.5-59.7% of the total carbon stock of the respective PA grass covered wooden houses (Table 7) indicating the absence of forests especially in the lowland PA. Moreover, the soil is the common below ground carbon stock to all landuses, and the total carbon stock of a landuse is mostly affected by the aboveground carbon stock.

Geo-climatic variables including altitude, precipitation and temperature of the study area were significantly correlated with above and below ground carbon storage of the studied land uses (p<0.07; r = ±0.999) (Table 8). Generally, wood carbon content increased as the density of wood of a species increased and both positively correlated significantly (p < 0.07; r = 0.47) (Table 8).

Soot organic carbon accumulation of wooden houses

The soot carbon was accumulated in the internal part of the roof of wooden houses that use solid biomass fuel for energy. The soot was stored temporarily and could be removed by clearing. In the studied lowland to highland PAs, a total of 3.93 - 12.68 g C m-2 yr-1 soot carbon was accumulated under the roof of wooden houses (Table 7) because of open stove fire used for cooking fuel. The soot carbon content of grass covered wooden house was higher than the corrugated iron sheet covered wooden houses in Daemir PA, which could be attributed to the confounding effect of grass in the soot (Table 7).

 

4. Discussion

Rural wooden houses as settlemets were surrounded by different landuses, mainly grazing land and scattered trees, which serve as carbon storage features. Wooden houses were storing biomass carbon in wood and grass, grazing lands were storing carbon in grass grass and soil, and scattered trees landuse in above ground stems, branches and leaves and belowground roots. Although soil carbon is the below ground carbon stock in all landuses considered, the results dealt only on the houses and trees with grazing land soil. During the study period, the natural forest was scanty in all the study sites due to reckless cutting and clearing for agricultural land, new settlements house construction and charcoal making. In lowland, there was remnant natural vegetation of Acacia and Combretum species. In midland and highland, there was Eucalyptus camaldulensis and E. globulus plantation, respectively. Species like C. africana, Ficus sur, J. procera, and P. falcatus were needed to make lumber for door and window of houses. These species were obtained locally in lowland and home gardens of midland but purchased from markets in the highland. Then preference of tree species used for house construction was determined by the availability of the species within the nearby forest or market as stated in Sheikh et al., (2009).

The availability of different tree/ shrub species of wood and the economic status of households determined the construction of different sized houses. The PA officials informed that, small houses were built by poor households and bigger houses by the riches. The decrease in the availability of grass due to land use change contributed to the construction of corrugated ironsheet covered houses. The shape of most of the grass covered houses was commonly with circular floor and conical roof as stated in other studies (Alemayehu, 2011) while the corrugate iron sheet covered houses were commonly with rectangular floor and triangular/ trapezoidal roof (Table 3). The type of wood used for construction of different parts of grass covered and corrugated iron sheet covered wooden houses was also different depending on the required strength of wood. For example, straight, long, strong and durable wood was commonly used for the central support (Axis) and surrounding wall as stated in other studies (Sarmiento et al., 2010) and the least strong wood was used for the roof, where there is no contact with soil (Table 2). The density and carbon content of wood of tree species used for house construction varied with diameter and stem position (Table 4) (Yeboah et al., 2013). Matured trees resulted in higher wood density and carbon stock than younger ones depending on moisture content, growth habit and health condition as confirmed in other studies (Dale, 2014; Kinyanjui, 2014). However, Martin, Doraisami, and Thomas (2018) showed that the wood carbon decrease as wood density increases. The overall mean carbon concentration of wood used for house construction in the present study, about 46.7% was in line with other studies (Chen et al., 2015; Djomo, Knohl, & Gravenhorst, 2011; Martin, Doraisami, & Thomas, 2018; Navaro et al., 2013; Yeboah et al., 2013), however, the minimum about 19.9% was lower than the 28% obtained in other study (Martin, Doraisami, & Thomas, 2018) which could be attributed to the young stems of low lignification. Therefore, further study is important on diameter of trees, wood density and their carbon concentration at different agrecologies and site condition.

The carbon stock of wooden houses was also determined by the type of woody species used for house construction and size of houses. In wooden houses, higher carbon storage was obtained in highland than lowland (Table 3) because of the temperature condition by which the highland is cold that require stronger and tightly constructed house with more wood, but the lowland is usually warm and dominated by temporarily constructed houses that require less durable biomass. However, a study conducted in Kwazulu, in South Africa, reported that the volume of wood of a house was greater in lowland than in highland situations (Liengme, 1983), which could indicate the use of voluminous woody branches and leaves in lowland. The carbon storage time of wooden house could be longer than a century if decay is hindered and protected from damages (Table 3). The above ground carbon storage in grass covered wooden houses in highland PA, and midland PA in the present study (46.1-49.26 kg C m-2) was higher than the study made by Churkina et al., (2010) (23-42 kg C m-2) in urban settlements and elsewhere in the world by Laganière et al., (2010), which could be attributed to the use of dense wood and the use of biomass for construction of the entire house. The carbon storage of wooden house could be more permanent sink than living trees in societies that use biomass energy by continuous cutting of trees deliberately as observed in the studied rural areas.

Carbon storage of different land uses varied with the type of geoclimatic (agroecology, or altitude) conditions. The relatively lower carbon stock obtained in grazing land soil and remnant scattered trees when compared to grass covered wooden houses opposes the previous results of Yin et al., (2012) and Gupta and Sharma (2013) because of dense wood used for rural house construction and high rate of deforestation. Although the carbon storage time for wooden house can be increased by different techniques that reduce wood decay to about a century, the carbon storage of soil is for millennia (Rumpel & Kögel-Knabner, 2010). In grazing land use, continuous grazing and natural annual lifecycle removed the grass in which case the above ground carbon stock was negligible and could not be taken as a perennial nor permanent carbon stock. That is the above ground grasses with short annual life added carbon to soil. The soil carbon in highland and lowland was lower than midland (Table 6), this might be due to rugged topographic nature of the highland that facilitate runoff and the higher temperature of the lowland that facilitate oxidation, which is in line with Demessie, Singh, and Lal (2016). The total carbon stock of landuses surrounding rural wooden houses that include grass covered wooden house decreased as the altitude decreased from highland (49.26 kg C m-2) to lowland (28.35 kg C m-2), and remnant woody plants from highland (29.4 kg C m-2) to lowland (2.68 kg C m-2) of the present study area as studied in Mwakisunga and Majule (2012) but opposes the total carbon stock studied by Simegn and Soromessa, (2015). The decrease in carbon storage with increased depth of soil (Table 6) was comparable with other studies carried out elsewhere (Tesfaye et al., 2016). At the end of 1m depth the highest carbon stock in midland as compared to the other agro-ecologies (Table 6) was attributed to the flat topography and the intermediate temperature level as stated in Xu, Dong, and Yang, (2017).

Low carbon stock of standing trees was obtained in lowland PA (Table 3) because of deforestation. Although, eucalyptus plantation in tropical conditions are highly productive, the frequent harvesting at faster rate of 5-10 years in midland of the present study hindered the maturity of stands of the standing live Eucalyptus camaldulensis, which reduced the carbon stock (Table 7) than the highland. The above ground carbon storage (Hairiah et al., 2010; IPCC, 2006) of E. globulus plantation in the highland of this study was higher than other studies (Berta, Soromessa, & Belliethathan, 2015), which can be attributed to long time conservation of live trees without cutting. Generally, the accumulation of higher carbon in grass covered wooden houses than either soil or remnant scatted trees landuse indicated the decline of forest cover (Table 7). There was strong correlation between the land uses and the carbon storage (p<0.05; r = ±0.999) (Table 8), indicating that carbon storage of an area is affected by the type of land use and agroecology as stated in other studies (England et al., 2016).

Soot carbon stock, as incomplete combustion of fuel could be as high as 1.268 * 10-2 kg m-2 (Table 7) in wooden houses, but it might not be permanent carbon stock if the roofs of wooden houses are kept clean continuously. The rural households responded that more soot was an indication of poverty. Soot is also the main indoor pollutant (IPCC, 2014). During the study period all the households encountered, informed that some member of the households face eye and breathing problems sometimes in life due to indoor pollution by soot and smoke. The soot accumulated contains sulfur and its health effect was very common (Fekadu, Bekele, & Feleke, 2017). Since wooden houses store carbon in constructed wood and soot more than soil and standing living trees (Table 7), it is important to consider these wooden houses carbon storage in climate change mitigation. Although rural wooden houses store carbon, the residents suffer from soot carbon indoor pollution. Therefore, wooden houses should be supported for the carbon stored by climate change financial mechanisms to solve the problem of indoor pollution.

The construction of wooden houses that use sustainably harvested biomass has no wastage of wood per se due to cutting of trees because rural areas usually use the residual biomass for energy (Sedjo, 2011). Other studies stated that houses built using wood and grasses are more cost and time efficient than those made of concrete and iron (Hurmekoski, 2017). Constructing houses using wood and grass is one way of offsetting emission as stated in other studies (Hurmekoski, 2017; Kayo, & Noda, 2018; Reid et al., 2004). Houses made of hollow concrete block can serve for over a century as close as to the wooden houses of about a century (personal communication). It was agrued that, using a combination of wood and concrete for house construction is important to offset emission in long staying houses by reducing decay, indoor pollution and deforestation.

 

5. Conclusions and Recommendations

The availability of wood from different tree species and economic condition of households determined the type and size of wooden house construction. Carbon content variation of different plant species, and different agroecologies resulted in different amount of carbon storage of land use per unit area. From the tree species used for house construction C. africana showed the highest carbon concentration (59. 2%) and Grewia species showed the highest wood density (0.92 g cm-3). The carbon storage time of wood used for house construction in the present study was 5-150 years depending on the type of house cover, agro-ecology, site condition and woody species. Rural grass covered wooden houses at a time stored 28.4-49.21 kg C m-2.

The total carbon stock of grazing land and its soil was 50.5-86.8% and the remnant scattered trees carbon was 9.5-59.7% of the total carbon stock of the respective PA grass covered wooden houses (Table 7). Therefore, carbon stock is shifting from forests to built structures, called rural wooden houses in human dominated landscapes, this may have an implication to distrupt the carbon stock, photosynthesis, and reduce oxygen supply. Wood harvesting for wooden house construction was one way of storing carbon outside the forest and wood residues left during house construction were used as firewood as the main sources of cooking energy that made no wastage of wood.

Carbon storages of grass in grazing land and soot in wooden houses were temporary because they can be removed by continuous grazing and cleaning, respectively. Although wooden houses store carbon, the residents were suffering from soot indoor pollution and deforestation, hence means of reducing indoor pollution, improving the house ventilation, introducing clean cooking technologies, increasing the life span of houses and afforestation measures should be practiced. The carbon stock of soot in midland was higher than the highland and lowland, which could be attributed to continuous indoor cooking in the presence of ample firewood. Avoiding wood decay through appropriate storage of wood in the cases of constructed wooden houses and the storage of leafy and bark residues that to be used as biomass energy should be trained to the rural people in order to reduce deforestation. In the future, it is important to identify methods of increasing the life span of wooden houses such as combining wood and iron / steel materials and cementing the basement parts in contact with soil to reduce decay. The field observation revealed that the indigenous tree species used for house construction were few inaddtion to the overall reduction of forest, and therefore, efforts should be strengthened to increase forest cover.

 

Acknowledgements

The research was financially supported by Hawassa University, Wondo Genet College of Forestry and Natural Resources, Central Ethiopia Environment and Forestry Research Center, and Association of African Universities Small Grant for Post Graduate Theses and Dissertations. We would like to thank Mehari Alebachew and anonymous reviewers for their valuable comments.

 

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