Project Global: Ground


This exploration of our current day metropolitan condition as a system of systems deals with the crust of the Earth as a primary carrying capacitor of human activities, from the extraction of resources deep within the ground, to agricultural operations that barely scratch the surface.

Part 1: Lexicon

Part 2: Atlas

Part 3: Architectural Projects


Part 3: Architectural Projects index

︎ By means of introduction...
    ︎ Parliament of Things
    ︎ Cemetery 36
    ︎ Institute of Mining Safety
    ︎ Post Thinkbelt   


︎ Extrapolated Realities     ︎ Co-Op Backyarding
    ︎ Informal Urban Farmers Market
    ︎ The Eviction Economy
    ︎ ASHES Base


︎ Symbiotic Infrastructure
    ︎ Stormwater Parks
    ︎ Agri-Course
    ︎ Dead & Alive

︎ Remediated Lands
    ︎ Anti-dust Landscape
    ︎ Soil & Green
    ︎ Rebound Landscape
    ︎ Nature’s Lung

︎ New Forms of Settlements
    ︎ Trickle-down Water Works
    ︎ Recycling Center    
    ︎ A.R.C.CA.DI.A
    ︎ Growing Roots

︎ Extraction Reaction

    ︎ Tailing Urbanism
    ︎ Lavoisier’s Law
    ︎ A New Energy Landscape
    ︎ Cake Town





The Existing Condition

Groundwater-Surface Water- Interactions


The analysis of the seasonal variations of groundwater and river water levels represents the conceptual model of the sand river aquifer system and the respective hydrological processes in dry season and flooding season. groundwater discharges into the river throughout most of the dry season. revealing the high permeability of the aquifer, groundwater levels are higher than the river level throughout the dry season. This means that harmful substances in groundwater are very easy to contaminate river water during dry periods. Water level rise during the flood season is extremely fast but temporary.Recharge occurs through quick infiltration from flood waters into very permeable sands, which are directly linked to the natural discharge of the sand river aquifer system to sustain the groundwater-surface water interaction after the rain season. However, after a long-term drought, the weathered sediment is easily washed away by the speed of the water flow, causing the flow and precipitation in the dry season, resulting in the depth of the river gradually becoming shallower in the next drought period,



Tutors 

Sanne van den Breemer
Filip Geerts
Ilmar Hurkxkens
Director of Studies

Salomon Frausto

Contributors

Nigel Alarcon(MX), Pooja Bhave(IN), Mariano Cuofano(IT), Fabiola Cruz(PE), Alonso Díaz(MX), Xiaoyu Ding(CN), Ines Garcia‑Lezana(ES), Sandra Garcia(ES), Martino Greco(IT), Sebastian Hitchcock(ZA), Alejandra Huesca(MX), Yesah Hwangbo(KR), Takuma Johnson(US), Yi-Ni Lin(TW), Paola Tovar(MX), Cristhy Mattos(BR), Preradon Pimpakan(TH), Adi Samet(IL), Raymond Tang(US), Kulaporn Temudom(TH), Danai Tsigkanou(GR), Jesse Verdoes(NL), Rongting Xiao(CN)