climate risk and vulnerability in the context of ......sesele sokotela, national soil surveys...
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CLIMATE RISK AND VULNERABILITY IN THE CONTEXT OF BUILDING
SOCIO-ECOLOGICAL RESILIENCE AND ADAPTATION
Theme: climate change, vulnerability, resilience,
measurement, adaptation
Sesele Sokotela, National Soil Surveys Programme –ZARI/MoAL
09 Jan 2013_Ibis Gardens, Chibombo
Notes on context key terms Climate risk –implies a measure of lack of predictability
in climatic conditions, leading to looming catastrophic set of situations for biota
Vulnerability –a state of lacking the ability to withstand or overcome a challenging condition or situation
Resilience –an ability to withstand and overcome a set of challenging conditions and situations
Adaptation –positive set of intervention mechanisms or practices developed as part of the custom for perpetual and sustainable survival by biota species
Measurement –determination of a condition or state of being by quantification of a threshold or level of quantity in objects using defined units and means
Presentation contents Vulnerability and Resilience Research • Highlights from southern and eastern Zambia • Indiana/Princeton Universities collaborative research with a
spatial variability assessment (GIS) dimension Soil Organic Carbon Measurements • Soil Organic Carbon Quantification Estimates in the Trans-
frontier Conservation Area (TFCA) of Western Zambia • UN-REDD+ mechanism Programme and ILUA II Project in
Zambia Adaptation
• Conservation Agriculture • Agriculture, Biodiversity and Forestry interfacing
Introduction
Concerns about Climate Change (global warming) and its associated subsequent results of occurrence of adverse weather
conditions on Earth (droughts and floods, etc.) are receiving great attention by various quarters of human society with varying views from the scientific community, policy makers and local communities of people
Greenhouse gases (GHGs) emissions to atmosphere are responsible (CO2 –an important culprit) Measurement for the amount of carbon (C) stored in soils (Soil Organic Carbon) is essential to help understand
dynamics of C cycling in terrestrial ecosystems (Biophysical variables) Socio-economic and Ecological systems vulnerability and resilience are also important to understand adaptation
factors
Importance of estimation of soil
carbon
Concerns about the rising quantities of carbon dioxide (CO2) in the atmosphere (0.5%yr-1)
Projected warming of world climate has hastened studies of Carbon (C) dynamics within known C pools emissions to the atmosphere (Lal et al., 2001)
IPCC, (1992) reported estimates of C fluxes to the atmosphere from land use changes amongst the most uncertain in quantifying C
Indications are that sinks for C, can be enhanced due to land use changes (e.g. forest re-growth, reforestation, CO2 fertilization and atmospheric N deposition effects (Watson et al, 1992; Hudson et al, 1994; Thornley et al., 1991)
Soil is recognised as one of the largest C reservoirs in the biosphere
In reported global C pools, SOC is about 2 to 3 times C more than in the atmosphere and terrestrial biota (Post et al, 1982; Eswaran et al., 1993)
Highlight results on “Effects of Agro-forestry plants in Soil Fertility Restoration and maize productivity in a degraded Miombo woodland in the Petauke district of eastern Zambia
Introduction
Vulnerability and Resilience of Social – Ecological Systems
research in Zambia being conducted to help elucidate issues pertaining to the mitigation of adverse effects of climate change in ecological systems
Zambia Agriculture Research Institute (ZARI)
Ministry of Agriculture and livestock (MoAL), in collaboration with the Research Institute for Humanity and Nature (RIHN) in conjunction with the Inter-University Research Institute Corporation and the National Institute for Humanities of Japan established a research site, Petauke in eastern Zambia
• Mwelwa village, area of Chief Sandwe of the Nsenga speaking people in the Petauke District, Eastern Province.
Purpose
study is aimed
to help add knowledge and find ways to remove conditions that undermine food security, soil ecology quality, and the natural environment health, in reference to climate change, with a particular focus for the local area or region, thereby provide for means to build both social and ecological resilience in the country
Objectives
Within Climate Change Context the study served as a trial and demonstration to evaluate the effectiveness of agro-forestry technologies and practices
in enhancing soil ecology resilience for crop productivity measured by the evaluation of effect of selected agro-forestry and green
manure plant species in soil fertility restoration demonstrate the named agro-forestry plants
species can restore and improve soil fertility conditions, and positively contribute to improved crop plant growth
measure soil property and characteristics
resulting from imposed agriculture cultural practices, like the use of agro-forestry technology
provide a platform foundation for assessment for socio-economic beneficial impacts that can be achieved by local
farming households on adoption of demonstrated technologies
Methodology
Locality approximately 400 km east of Lusaka Great East Road, Petauke District about 40 km to the north of the Petauke on the Ukwimi Road, at Mwelwa village in Chief Sandwe’s
area Selection criterion noted prevalent high levels of forest and soil degradation by preliminary studies on the physical ecology with application of Remote Sensing techniques and review of climatic, vegetation, geology, soils and land use
information available
land through local consultations with the traditional leadership and communities at
various appropriate fora e.g. meetings, about 20 ha land allocation for field research on a
relatively virgin site both RIHN and ZARI are at the site engaged in conducting field research studies presentation concerns the ZARI trial and demonstrations
treatments
six treatments
imposed, each replicated three times in a randomized complete block design (RCBD)
A Grilicidia sepium fallow (Gs) B Maize (Zea mays) continuous fertilizer
(MF1) C Native Forest fallow (NF) D Maize, no Fertilizer (MF0) E Mucuna pruriens (Velvet bean) green
manure fallow (BV) F Cajanus cajan (pigeon pea) fallow (Pp)
Soil measurement and sampling
each field plot 20m x20m
soils were sampled at two depths, namely, the top soil (0-20) cm, and subsoil (40–60) cm depths
Soil parameters analyzed for chemical and physical soil properties
pH, Bases (Ca, Mg, K, and Na), cation retention capacity (CEC), soil Organic Carbon (C%), total Nitrogen (N%), available Phosphate (P ppm), Particle Size Distribution (PSD), Bulk density (BD)
Land preparation
All cultivated had plots initial land preparation
cutting down and stumping trees found on the site
digging with hand hoes well before the onset of the rainy season in October
soil samples taken at the prescribed top and sub soil depths
Biomass estimation
Above ground plant biomass in the agro-forestry and native fallow plots was estimated
by measuring plant height
and stem girth (diameter) at ground collar level
Field Days
Purpose for hosting the field days
to demonstrate and disseminate improved agro-technology and soil fertility management information
for the local community
share a platform of understanding and appreciation of research activities conducted and promoted in the area
a first field day was held in March 2009
second field day was held in April 2011
to show case developments of the research trials and demonstrations being conducted at the research site
Results highlights
study area forms part of the eastern plateau
on eastern shoulder of the Luangwa Rift Valley ecology system
the study site is in Agro-Ecological Region IIa (east of the Luangwa River)
Mpika
Solwezi
Sesheke
Kaoma
Serenje
Kalabo
Chama
Mkushi
Mumbwa
Kasempa
Lukulu
Chinsali
Mwinilunga
Kalomo
Senanga
MufumbweZambezi
Lundazi
Kaputa
Kazungula
Isoka
Kabompo
Mansa
Mongu
Mbala
Nyimba
Itezhi-Tezhi
Shangombo
Samfya
Kasama
Chibombo
Chongwe
Mungwi
Kapiri Mposhi
Luwingu
Mporokoso
Petauke
Kafue
Choma
Lufwanyama
Mpongwe
Mpulungu
Chipata
Mwense
Kawambwa
Milenge
Monze
Mazabuka
Mambwe
Chilubi
Namwala
Katete
Chavuma Masaiti
Chiengi
Nakonde
Gwembe
Luangwa
Siavonga
Sin
azo
ngw
e
Nchelenge
Chadiza
Kabwe
Livingstone
Lusaka Urban
Chililabombwe
MufuliraChingola
Kalulushi Kitwe
Luanshya
Ndola
200 0 200 400 Kilometers
N
EW
S
Agro-Ecological Regions
District boundary
KEY
Source: Soil Survey, Mt. Makulu ChilangaDecember 2002
Scale 1: 2,500,000
Regions
I
IIa
IIb
III
LEGEND
Annual rainfall ranges between 750 to1000 mm
a crop growing period of 90-150 days
major soils are largely Lixisols, Luvisols, Alisols, Acrisols, some Leptosols, and Vertisols in low lands (Soil Survey Section, 1991).
Soil Classification
Initial soil characterization classified as Typic Plinthustalfs (Soil Survey Staff, 2000), or Plinthic Luvisols ( FAO, 1999)
soil profile comprises a darkish brown sandy clay loam topsoil, fine reddish brown subsoil and gravelly in the lower horizons below 90 cm depth in the pedon
Soil properties
the soils were low to medium in soil fertility
Soil reaction conditions were of strong to medium acidity (pHKCl 5.1 – 5.7)
low organic C content (<2.0 %),
low N and P content,
BSP low to medium
Sample soil properties at research site
Parameter Mean SD CV
Total N (%) 0.8 0.02 28.7
Total C (%) 1.24 0.47 38.0
pH (H2O) 6.3 0.2 3.5
pH (KCl) 5.5 0.3 5.2
Sand (%) 72.9 3.4 4.7
Clay (%) 12.6 2.5 20.1
Bulk Density (Mgm3) 1.3 0.1 8.6
Soil fertility status
soil fertility indicator parameters
measured at each research/demonstration plot in
top soil (0 -20 cm)
sub soil (40 -60 cm) depths
soil fertility condition (year 2010)
Topsoil Mean LSD SE
Total Carbon (%) 0.71 0.71 0.22
CEC (ppm) x
K (ppm) 185.6 60.5 19.2
Ca (ppm) ?
Mg (ppm) 135.6 70.4 22.3
Na (ppm) 38.9 18.7 5.9
P (ppm) ?
pH (CaCl2) 5.3 0.66 0.21
Subsoil Mean LSD SE
CEC (ppm) 10.6 3.3 1.5
Ca (ppm) 456 330.8 105.0
K (ppm) 197.8 66.5 21.1
Mg (ppm) 138.9 67.6 21.4
Na (ppm) 46.2 63.5 20.1
P (ppm) 9.8 7.1 1.3
pH (CaCl2) 5.4 0.43 0.14
Initial field soil condition
soil fertility field conditions showed no significant differences across the imposed treatments
soil types were relatively uniform in soil fertility
maize crop was imposed over all treatment trial field subplots
to appreciate effects of farming practice technologies (agro-forestry, etc.)
@50 % of the recommended fertilizer rate (mTF1/2)
@ and no fertilizer use (mTFo)
Maize Biomass at Harvest (Kg) Maize Biomass at Harvest (Kg) with half and zero fertilizer rates (mTF1/2 & Fo)
Plot no. Treatment Rep Block Biomass (mTFo) mTF1/2
1 B 1 9.81 37.14
2 C 1 12.65 33.65
3 E 1 5.14 30.66
4 F 1 20.12 43.24
5 D 1 14.76 39.53
6 A 1 21.28 50.16
7 F 2 10.53 31.88
8 B 2 12.84 37.28
9 E 2 6.28 45.06
10 D 2 9.18 28.18
11 C 2 3.72 17.9
12 A 2 21.24 33.7
13 F 3 12.58 44.02
14 D 3 8.4 25.02
15 A 3 14.32 48.28
16 C 3 3.92 33
17 B 3 13.08 37.56
18 E 3 10.46 37.64
Agro-forestry demonstration performance (@2 years)
Plant sp. C. cajan G. sepium N. forest
Height (m) 3.66 2.04 3.06
Girth (mm) 43.54 43.7 51.78
Trees growth performance at 2 years
0
0.5
1
1.5
2
2.5
3
3.5
4
1
Technology practice
Heig
ht
(m)
C. cajan
G. sepium
N. forest
Trees diameter at stem ground collar
C. cajan
G. sepium
N. forest
Highlights from social-ecological Resilience and vulnerability Research in southern Zambia
(RIHN/ZARI Collaborative study)
Objective
The main objective is two-fold:
to gather detailed socio-economic data information on the identified local households in the community,
undertake some biophysical data through field experiments, to help guide not only intervention actions in the context of climate change,
but facilitate future government policy with regard to food security
Study site location
LAKE KARIBA (A)
ZAMBEZI ESCAPMENT
CHOMA PLATEAU
Weather Station installed @ sites A and C
AUTOMATIC WEATHER STATION
Local Agricultural Production
Summary of results (Site A)
Site B Rainfall
Site C Rainfall
All sites showed above normal rain
Socio-economic factors
Body Mass Index for Men and Women
Conclusion
Observed precipitation in the rainy seasons showed different intra-seasonal variations.
Households and their communities do show remarkable local social resilience to shocks
Recommendation
Further studies are needed to clarify strategies to adapt to climate change and maintain food security
Highlights On Soil Organic Carbon
Quantification Estimates In The Trans-frontier Conservation Area Of
Western Zambia
Climate Change Programme in Collaboration with PPF, RSA
The Study Area
Fro the southern Africa sub-continent PPF’s Climate Change Programme aimed to assist host countries (Angola, Botswana, Malawi, Mozambique, Namibia, Swaziland, Zambia, and Zimbabwe)
To provide an economic driver to help reduce deforestation in the TFCAs
restore degraded areas
and provide improved livelihoods for local communities of people
the initiative would also provides a platform for exploring means to benefit from the international carbon market
Pilot site for the Location maps showing the Kaza-Zambia TFCA Study Area
Because soil comprises a major source and sink for atmospheric CO2 the characterization, measurement and quantification of soil organic pools are of significant importance
Soil organic carbon is commonly characterized by various carbon components present in the soil The complexity and diversity of soil organic matter physical and chemical composition are recognized As such careful identification and selection of methods for the quantification and estimation of the content of SOC is critical
Study sites in western Zambia
The study site land area assessed constituted approximately 1.5 million hectares or about 15,000 km2 in size
The area stretched from Mulobezi in the east, to Sinjembela in the west, Sioma in the north, and Katima Mulilo to Imusho in the south. The Zambezi River bisects the study area
The vegetation ranges from open Burkea africana woodlands to tall, closed Baikiaea purijuga woodlands, Brachystegia spp. woodlands, Acacia spp. woodlands, open grasslands and floodplains on deep Kalahari sands (Hansen et al. 2002)
For a detailed description of vegetation, soils and geology also see Trapnell (2001), Edmonds (1976), and D.O.S. (1970)
Objectives
Soil carbon stock quantification has the main objective to estimate changes in soil organic carbon in
the study area serve as a means for designing and the development of a
methodology to help establish a threshold of baselines of carbon stock
quantification in the Kaza-Zambia Transfrontier Conservation Area (TFCA) in the Western Province of Zambia
As part of a development objective PPF provided means for conservation and management of vast
wilderness areas, add connectivity and robustness to ecosystems and contribute to the improvement of the livelihood of rural people
Methods
Conducted in the Kaza-Zambia TFCA in western Zambia from 18 May 2009 to 16 June 2009
multidisciplinary-participatory and collaborative exercise for carbon stock quantification in the area, and was spearheaded by the Peace Parks Foundation of South Africa
Zambia key participating and collaborating institutions comprised the Forestry Department (FD) and Zambia Wildlife Authority (ZAWA), Ministry of Tourism, Environment and Natural Resources (MTENR), presently, Ministry of Lands and Natural Resources , and
Environmental Protection (MLNREP) Zambia Agriculture Research Institute (ZARI) of the Ministry of Agriculture and Livestock (MoAL), formerly, Ministry of Agriculture
and Cooperatives (MACO)
The study focused development of Conservation Agriculture management practices Carbon sequestration consequences, especially, adaptation and development of methods and techniques for field sampling, data
capturing, and taking measurements of terrestrial carbon content in study areas
Thus, much effort was devoted to the development of methods to help estimate baselines for quantification of Soil Organic Carbon stocks in pilot study sites from western Zambia
Prevailing climatic conditions
Water balance diagram for Sesheke Temperature (oC)
Soil Organic Carbon Assessment
Calculation of total carbon five main pools may be identified, namely,
1) live and dead standing tree trunks,
2) tree parts excluding trunks, but including canopy and coarse roots (diameter >2 mm),
3) vegetation other than trees,
4) other woody debris and forest floor, and
5) mineral soil organic matter (including faunal and floral materials and roots <2 mm diameter)
Soil organic carbon measurements The current study, calculated C in successive soil layers of 0 – 5 cm, 5 – 10 cm and 15 – 20, respectively
Thus -a specified soil depth of 20 cm over the unit land area equivalent to one square kilometer
Mg mass value
Estimation of soil organic carbon For the TFCA pilot site study area of western Zambia the areal calculation (Grossman et al., 2000)
applying the general equation for summation of soil organic carbon (SOC) by 5 cm soil layers on an areal basis was employed equation:
SOC ₌ L1 x SOCP1 x p1 (1-V>21 )/100 + L2 x SOCP2 x p2 (1-V>22 )/100 + … • ____________________________________________________
10
• Where, SOC ₌ Soil Organic Carbon in Kg m-2 SOCP ₌ Soil Organic Carbon percentage (laboratory determined) L ₌ Thickness of the soil layer in cm (measured in soil profile) p ₌ Moist bulk density of the < 2 mm soil fabric (at 33 kPa suction V>2 ₌ Volume percent soil coarse fragments greater than 2 mm diameter for our purpose soil organic carbon is the mass of carbon stored in the soil per square kilometer
SOC ₌ MC ₌ Mg C km-2 to 20 cm • Where, SOC is soil organic carbon MC is Mass organic carbon storage in soil Mg C km-2 is 1000 g carbon mass per square kilometer or Kg of carbon in a land unit area of one sq.
km of the soil layer to 20 cm depth from the ground surface
Field soil sampling
Field soil sampling for carbon stock was conducted in the Kaza Zambia TFCA in the Western Province of Zambia across
50 sample plots randomly selected on local locations from
Mulobezi, Sesheke, Sioma, Sinjembela and Imusho, study sites
At each study site (Cluster)
several sample plots were visited and physically sampled as locations of study sites
Location of study site points
Cluster sites locations
The study sites were treated as sample clusters, namely,
1 Mulobezi,
2 Sesheke,
3 Sioma,
4 Sinjembela ,
5 Imusho
1
2
3
4
5
Soil properties
Soil Texture (Plots 11 – 21)
Soil Texture (Plots 31 – 43)
Dominance of the sand fraction, the fine and medium sand grain size was
consistent with the nature of the Kalahari sand parent materials from
which the local soils were formed Spaargaren, (1987) asserts that the whole sand fraction is quartz
Mulobezi sample data
Study Plot Study Site SOC (Mass Mg C /sq. km pH (CaCl2) Org C % N % Texture Class Elevation
1 MULOBEZI X 5.1 0.168482 0.18 Sand 994 2 MULOBEZI 1745.3 5.5 0.094022 0.012 Sand x 3 MULOBEZI 3702.4 5 0.216398 0.022 Sand x 4 MULOBEZI 4187.2 4.7 0.221488 0.026 Sand 973 5 MULOBEZI 4158.5 4.6 0.255563 0.02 Sand 971 6 MULOBEZI 2632.5 4.6 0.215467 0.023 Sandy Loam 994 7 MULOBEZI 6374.4 4.5 0.304993 0.032 Sand x 8 MULOBEZI 5904.6 5.1 0.295948 0.0501 Sandy Loam 960 9 MULOBEZI 3519.6 4.8 0.295948 0.028 Sand x 10 MULOBEZI 5088.1 4.6 0.333507 0.024 Sandy Clay Loam 1000
pH and SOC levels in study sites
Soil reaction SOC Levels
Result highlights
Sioma and Sinjembela with mean values of SOC about 2,373 and 2,650 Mg C km-2 _ 20 cm, respectively, had substantial levels of human
settlement activities In the Sioma area arable agriculture such as subsistence crop farming (maize, sorghum and pearl
millets cultivation) were prominent Sinjembela area, in addition to crop cultivation, cattle rearing were also an important farming
activity Mulobezi area (mean SOC content about 4,100 Mg C km-2 _ 20 cm) is well settled by local people, but a number of Protected Forest reserves were in existence and
the area is also an important regulated timber harvesting concession region The Sesheke area (3,210 Mg C km-2 _ 20 cm) proximity to a prominent urban center, and where protected forest reserves exist, timber
harvesting activities take a significant prominence A high SOC value (4,659 Mg C km-2 _ 20 cm) in Imusho area seems to be associated with low
levels of human settlement and forms part of the Sioma-Ngwezi National Park
It was observed that Land Use and Land Use Changes may have influence on Soil Organic Carbon of local areas
Recommendation
Similar comparative and verification studies be conducted in other areas than the KAZA
Trials and Demonstration research may be conducted involving local communities of people for adaptation productivity in prevailing environments
SOIL SURVEY DESIGN AND METHODOLOGY DEVELOPMENT
Introduction
Zambia is developing a national strategy and action plan to reduce deforestation and land degradation
In order to develop an effective national forest resources monitoring system, baseline data and information are needed to be in place to serve as reference levels
In this regard the United Nations Reduction of Emissions from Deforestation and forest Degradation (UN-REDD) programme for Zambia is undertaking an active implementation phase since its approval by the UN-REDD Policy Board for implementation in 2010
The effective implementation is supported by the U.N. Agencies (FAO, UNDP, and UNEP) as part of the partnership with the Government of Zambia
Main outcomes of the project
Strengthened capacity to undertake planning and implementation of Sustainable Forest Management and Reduced Emissions from Deforestation and Forest Degradation (SFM & REDD) through:
better information provisions,
institutional capacity building, information dissemination improved multi-sector dialogue within the country and internationally
Outputs from the programme implementation are threefold: effective information dissemination and use improved methodology regarding : human resource capacity development, data capture and analysis, forest resources inventory, and provide information for sustainable forest management (SFM), monitoring of REDD, undertake carbon stocks inventory, facilitate the implementation of the REDD+ mechanism and ILUA II through : mapping and field surveys
Objectives
The main objective of the present assignment is to help estimate soil carbon stocks through the development of a soil survey design and methodology for conducting field soil samples collection, Define procedure for carrying out laboratory analytical tests, and undertake to facilitate soil data interpretations and
information dissemination for the implementation of the UN-REDD & ILUA II project under the
Forestry Department in Zambia And produce, a manual to serve as standard instruction to guide
soil carbon survey sampling design and laboratory analysis methodology
Manual for soil carbon survey assessment
A manual for soil carbon survey was designed as standard guideline for conducting assessments and monitoring of soil carbon is provided in two parts and includes the following main contents
Part I -field soil sampling procedures and Part II -soil laboratory analysis
methodological procedures
Procedural protocol
The Manual sets out the procedural protocol to be followed for consistency in measurement, reporting and verification concerning carrying out the inventory soil organic carbon stocks covering the entire country in Zambia
Developed Pre-proposal: Promoting Resilient Farming Technologies Against A Changing Climate Amongst Vulnerable Rural Farmers In Zambia
Goals and Objectives The overall goal of the project is to improve capacities
for farmers to fight against poverty and hunger in the nation through the adaptation of soil fertility and water management technologies and best practices available from agricultural research and extension services
Therefore, in the end the development and provision of improved agricultural technologies and sustainable use of soils, land and water resources are to help build capacity for rural farmers in poverty alleviation and achieving food security by interfacing Agricultuture, Biodiversity and Forestry
SOIL CARBON STOCK INVENTORY AND MONITORING: TRAINING AND FIELD MANUAL FOR SOIL SAMPLING
2012
Forestry Department LUSAKA
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