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Tracking Carbon Dynamics by Sources, Sinks, and Removals in Malawi’s Land Use, Land-Use Change, and Forestry (LULUCF) Sector to Enhance Carbon Market Development
Edward Missanjo
,Henry Kadzuwa
Posted: 19 January 2026
Adaptation or Resistance: How Trust in Public Environmental Agencies Influences Farmers’ Climate Change Responses
Nicole Torres-Torres
,José Luis Llanos
,Leyla Meneses
,Maximiliano Rosales-Vergara
,Aracely Burgos
,Juan Carlos Alano
,Catalina Astudillo
,Claude Garcia
,Cristian Leyton
,Loreto F. Fuenzalida
+2 authors
Posted: 19 January 2026
Open Access Accumulation Chambers SAGE (Surface – Air Gas Exchange) – DIY Philosophy
Bartosz M. Zawilski
,Vincent Busitllo
Posted: 19 January 2026
Satellite-Based Innovative Methodological Procedure for Estimation of Daily Actual Crop Evapotranspiration in Vulnerable Agroecosystems: A Case Study in Castilla-La Mancha, Spain
Marios Spiliotopoulos
,Nicolas R. Dalezios
,Nikolaos Alpanakis
,Georgios Tziatzios
,Ioannis Faraslis
,Stavros Sakellariou
,Pantelis Sidiropoulos
,George Karoutsos
,Apostolos Tsiovoulos
,Konstantina Giannousa
+4 authors
Posted: 19 January 2026
Associations Between Temperature and Precipitation Variability and Malaria Incidence in Sub-Saharan Africa: A Systematic Review and Meta-Analysis
Ishmael Yaala
,Michael Osei Adu
,Frederick Ato Armah
Posted: 19 January 2026
An Integrated Sedimentological and Ecological Approach for Investigating Vulnerable Coastal Lakes: A Case-Study
Roberta Somma
,Mohammadali Ghanadzadeh Yazdi
,Majed Abyat
,Raymart Keiser Manguerra
,Salvatore Zaccaro
,Antonella Cinzia Marra
,Salvatore Giacobbe
Posted: 19 January 2026
Earliest Evolved Rocks: A Solar System Perspective
Sheng Shang
Posted: 19 January 2026
Electronic Waste-Associated Lead Exposure and Child Neurodevelopment in Sub-Saharan Africa: A Systematic Review and Meta-Analysis
Ishmael Yaala
,Michael Adu Osei
,Frederick Ato Armah
Posted: 19 January 2026
Democratizing Plastic Governance Through Effective Engagement of Grassroots Communities
Ahmed Tiamiyu
,Jubril Gbolahan Adigun
Posted: 19 January 2026
The Optimal Model for Living Walls in South Africa: A Quantity Surveying Perspective
Rolien Terblanche
,Samuel De Witt
,Aiden Pringle
Posted: 16 January 2026
Assessing the Economic Impact of Irrigation Modernization Projects: A Case Study from Türkiye
Gokmen Dedemen
,Salih Kocak
Posted: 16 January 2026
Prediction of Air Pollutants based on Time-Weighted Ensemble Model and Adaptive Air Quality Index Model
Borui Wang
,Chenjie Gong
,Chao Liu
,Jiahe Yang
,Huili Huang
Posted: 16 January 2026
Ecosystem-Based Adaptation Practices for Climate Resilience: Evidence from Smallholder Farmers’ Perceptions of Co-Benefits and Adoption Decisions in Mabalane District, Mozambique
Jaime Carlos Macuácua
,Nicia Giva
,Claudius Patrick Waran
Posted: 16 January 2026
Germination Potential of Stored and Freshly Harvested Seeds of Mandacaru (Cereus Jamacaru DC)
Hugo Roldi Guariz
,Gabriel Danilo Shimizu
,Eduardo Inocente Jussiani
,Diego Genuário Gomes
,Kauê Alexandre Monteiro
,Huezer Viganô Sperandio
,Marcelo Henrique Savoldi Picoli
Knowledge about the germination potential of Mandacaru seeds is fundamental for maintaining breeding programs and germplasm banks. Thus, we aimed to study the germination of stored and freshly harvested mandacaru seeds in order to investigate seed viability as a function of storage imposition, in addition to characterizing seed anatomy and conducting biochemical evaluation. Germination tests were conducted in a completely randomized design in a 2×6 factorial scheme, with two storage conditions and six temperatures (15, 20, 25, 30, 35, and 40°C), with 4 replications of 25 seeds each. Anatomical evaluation tests and biochemical tests had 5 and 10 replications for each storage condition, respectively. It is concluded that the range of 25-35°C is ideal for germination of C. jamacaru seeds, and temperatures below 20°C and above 35°C are detrimental to germination. X-ray computed microtomography was efficient for characterizing seed anatomy and differentiating their tissues, allowing accurate and clear evaluation of their internal structures, and proper storage was efficient in minimizing the deleterious effects of H₂O₂ and MDA accumulation.
Knowledge about the germination potential of Mandacaru seeds is fundamental for maintaining breeding programs and germplasm banks. Thus, we aimed to study the germination of stored and freshly harvested mandacaru seeds in order to investigate seed viability as a function of storage imposition, in addition to characterizing seed anatomy and conducting biochemical evaluation. Germination tests were conducted in a completely randomized design in a 2×6 factorial scheme, with two storage conditions and six temperatures (15, 20, 25, 30, 35, and 40°C), with 4 replications of 25 seeds each. Anatomical evaluation tests and biochemical tests had 5 and 10 replications for each storage condition, respectively. It is concluded that the range of 25-35°C is ideal for germination of C. jamacaru seeds, and temperatures below 20°C and above 35°C are detrimental to germination. X-ray computed microtomography was efficient for characterizing seed anatomy and differentiating their tissues, allowing accurate and clear evaluation of their internal structures, and proper storage was efficient in minimizing the deleterious effects of H₂O₂ and MDA accumulation.
Posted: 15 January 2026
Post-Collisional Cu-Au Porphyry and Associated Epithermal Mineralisation in the Eastern Mount Isa Block: A New Exploration Paradigm for NW Queensland
Kenneth D. Collerson
,David Wilson
Post-collisional Cu-Au-Ni-Co-Pt-Pd-Sc porphyry, [Duck Creek porphyry system (DCPS)], with overlying Au-Te-Bi-W-HRE epithermal mineralisation, [Highway epithermal system (HES)] has been discovered in the core of the Mitakoodi anticline, southwest of Cloncurry. Xenotime and monazite geochronology indicates mineralisation occurred between ~1490 and 1530 Ma. Host rock lithologies show widespread potassic and/or propylitic to phyllic alteration. Paragenesis of porphyry sulphides indicate early crystallisation of pyrite, followed by chalcopyrite, with bornite forming by hydrothermal alteration chalcopyrite. Cu sulphides also show the effect of supergene oxidation alteration with rims of covellite, digenite and chalcocite. Redox conditions deduced from V/Sc systematics indicate that the DCPS contains both highly oxidized (typical of porphyries) and reduced lithologies, typical of plume generated tholeiitic and alkaline suites. Ni/Te and Cu/Te systematics plot within the fields defined by epithermal and porphyry deposits. Duck Creek chalcophile and highly siderophile element (Cu, MgO and Pd) systematics resemble data from porphyry mineral systems, at Cadia, Bingham Canyon, Grasberg, Skouries, Kalmakyr, Elaisite, Assarel and Medet. SAM geophysical inversion models suggest the presence of an extensive porphyry system below the HES. A progressive increase in molar Cu/Au ratios with depth from the HES to the DCPS, supports this conclusion. Three metal sources contributed to the DCPS-HES viz., tholeiitic ferrogabbro, potassic ultramafic to mafic system and a Fe and Ca-rich alkaline system. The latter two imparted non-crustal superchondritic Nb/Ta ratios that are characteristic of many deposits in the eastern Mount Isa Block. The associated tholeiite and alkaline magmatism reflect mantle plume upwelling through a palaeo-slab window that had accreted below the eastern flank of the North Australian craton following west verging collision by the Numil Terrane. Discovery of this linked mineral system provides a new paradigm for mineral exploration in the region.
Post-collisional Cu-Au-Ni-Co-Pt-Pd-Sc porphyry, [Duck Creek porphyry system (DCPS)], with overlying Au-Te-Bi-W-HRE epithermal mineralisation, [Highway epithermal system (HES)] has been discovered in the core of the Mitakoodi anticline, southwest of Cloncurry. Xenotime and monazite geochronology indicates mineralisation occurred between ~1490 and 1530 Ma. Host rock lithologies show widespread potassic and/or propylitic to phyllic alteration. Paragenesis of porphyry sulphides indicate early crystallisation of pyrite, followed by chalcopyrite, with bornite forming by hydrothermal alteration chalcopyrite. Cu sulphides also show the effect of supergene oxidation alteration with rims of covellite, digenite and chalcocite. Redox conditions deduced from V/Sc systematics indicate that the DCPS contains both highly oxidized (typical of porphyries) and reduced lithologies, typical of plume generated tholeiitic and alkaline suites. Ni/Te and Cu/Te systematics plot within the fields defined by epithermal and porphyry deposits. Duck Creek chalcophile and highly siderophile element (Cu, MgO and Pd) systematics resemble data from porphyry mineral systems, at Cadia, Bingham Canyon, Grasberg, Skouries, Kalmakyr, Elaisite, Assarel and Medet. SAM geophysical inversion models suggest the presence of an extensive porphyry system below the HES. A progressive increase in molar Cu/Au ratios with depth from the HES to the DCPS, supports this conclusion. Three metal sources contributed to the DCPS-HES viz., tholeiitic ferrogabbro, potassic ultramafic to mafic system and a Fe and Ca-rich alkaline system. The latter two imparted non-crustal superchondritic Nb/Ta ratios that are characteristic of many deposits in the eastern Mount Isa Block. The associated tholeiite and alkaline magmatism reflect mantle plume upwelling through a palaeo-slab window that had accreted below the eastern flank of the North Australian craton following west verging collision by the Numil Terrane. Discovery of this linked mineral system provides a new paradigm for mineral exploration in the region.
Posted: 15 January 2026
A Comparative Review of Life-Cycle Assessments of Treatment Strategies for Swine Slurry with a Focus on Anaerobic Co-Digestion
Pedro Esperanço
,António Ferreira
,José Ferreira
Posted: 15 January 2026
Climate Change Impacts on Agricultural Landscapes in the Fergana Region: Assessment and Adaptation Strategies
Ozodxon Mahmudovna Qoʻziboyeva
,Jamshid Abduhalilovich Mahkamov
,Nargiza Muzaffarovna Babayeva
,Zarina Boytemirova
Posted: 15 January 2026
Mechanisms of Accumulation–Transport–Discharge and Source Apportionment of Combined Sewer Overflow Pollution
Xiaolong Li
,Zhiwei Zhou
,Haifeng Jia
,Zhili Li
,Zhiyu Yang
,Zibing Cai
,Hongchi Zhou
,Xiaoyu Shi
Combined sewer overflow (CSO) pollution has consequently become a critical challenge, yet its formation depends on tightly coupled dry-and-wet weather processes. This study aims to integrate high-resolution field monitoring with statistical analysis to characterize the full “accumulation-transport-discharge” cycle of CSO pollution. Results indicated that during dry periods, domestic sewage exhibited strong enrichment, with concentrations of TIN, COD, and TP being 2.1-, 2.3-, and 1.9-fold higher, respectively, than the Chinese secondary discharge standards (GB 18918-2002). Surface sediment showed pronounced spatial heterogeneity, with greater loads in residential than transportation areas and substantial fine-particle accumulation on roofs (particle size <150 μm, accounting for 73% by mass). Sewer sediments, dominated by coarse inorganic particles (over 77% by mass), represented the main pollutant reservoir. Rainfall produced distinct hydrodynamic and water-quality responses. Light rain following long antecedent dry periods generated a high-concentration but low-load regime with a strong first flush, whereas moderate rain yielded lower concentrations but higher loads. Overflow occurred when rainfall exceeded ~14 mm, with pollutant peaks lagging rainfall by 20–45 min in the studied area. TIN and TP peaked sharply at rainfall event onset, and first-flush intensities followed TIN > TP > COD > SS. Source apportionment identified sewer sediments as the dominant CSO source, followed by surface runoff and domestic sewage. These findings clarify the mechanisms linking dry-weather accumulation to wet-weather transport and support targeted CSO pollution control and urban water-quality management.
Combined sewer overflow (CSO) pollution has consequently become a critical challenge, yet its formation depends on tightly coupled dry-and-wet weather processes. This study aims to integrate high-resolution field monitoring with statistical analysis to characterize the full “accumulation-transport-discharge” cycle of CSO pollution. Results indicated that during dry periods, domestic sewage exhibited strong enrichment, with concentrations of TIN, COD, and TP being 2.1-, 2.3-, and 1.9-fold higher, respectively, than the Chinese secondary discharge standards (GB 18918-2002). Surface sediment showed pronounced spatial heterogeneity, with greater loads in residential than transportation areas and substantial fine-particle accumulation on roofs (particle size <150 μm, accounting for 73% by mass). Sewer sediments, dominated by coarse inorganic particles (over 77% by mass), represented the main pollutant reservoir. Rainfall produced distinct hydrodynamic and water-quality responses. Light rain following long antecedent dry periods generated a high-concentration but low-load regime with a strong first flush, whereas moderate rain yielded lower concentrations but higher loads. Overflow occurred when rainfall exceeded ~14 mm, with pollutant peaks lagging rainfall by 20–45 min in the studied area. TIN and TP peaked sharply at rainfall event onset, and first-flush intensities followed TIN > TP > COD > SS. Source apportionment identified sewer sediments as the dominant CSO source, followed by surface runoff and domestic sewage. These findings clarify the mechanisms linking dry-weather accumulation to wet-weather transport and support targeted CSO pollution control and urban water-quality management.
Posted: 15 January 2026
Evaluating Geostationary Satellite–Based Approaches for NDVI Gap Filling in Polar-Orbiting Satellite Observations
Evaluating Geostationary Satellite–Based Approaches for NDVI Gap Filling in Polar-Orbiting Satellite Observations
Han-Sol Ryu
,Sung-Joo Yoon
,Jinyeong Kim
,Tae-Ho Kim
Posted: 15 January 2026
AI Transparency and Climate-Adaptive Agritourism: Farm-Level Decision-Making and Rural Resilience
Aleksandra Vujko
,Nataša Perović
,Vuk Mirčrtić
,Adriana Radosavac
,Darjan Karabašević
Posted: 15 January 2026
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