Verflüssigungsrisiko-Rechner

Schätzen Sie die Wahrscheinlichkeit der Bodenverflüssigung basierend auf Erdbeben-Parametern und Bodenbedingungen.

Assessment

Bodenverflüssigung bei Erdbeben verstehen

Bodenverflüssigung tritt auf, wenn wassergesättigter, lockerer, körniger Boden während Erdbebenerschütterungen seine Festigkeit und Steifigkeit verliert und sich wie eine Flüssigkeit statt wie ein Feststoff verhält. Wenn seismische Wellen durch wassergesättigten Sand oder Schluff laufen, erhöhen sie den Wasserdruck zwischen den Bodenteilchen (Porenwasserdruck). Steigt dieser Druck so weit an, dass er dem Gewicht des darüberliegenden Bodens entspricht, verlieren die Teilchen den Kontakt zueinander und der Boden fließt vorübergehend wie eine zähe Flüssigkeit. Dieses Phänomen kann dazu führen, dass Gebäude einsinken, kippen oder einstürzen; unterirdische Strukturen wie Rohre und Tanks an die Oberfläche schwimmen; und Hänge durch seitliche Ausbreitung versagen.

Der Standard-Penetrationstest (SPT) N-Wert ist eine wichtige Feldmessung zur Bewertung der Verflüssigungsanfälligkeit. Er misst die Anzahl der Hammerschläge, die erforderlich sind, um ein Probenahmerohr 30 cm in den Boden zu treiben – höhere N-Werte deuten auf dichteres, widerstandsfähigeres Material hin. Böden mit SPT-N-Werten unter 15 bei gesättigten Bedingungen gelten im Allgemeinen als verflüssigungsanfällig. Die Grundwassertiefe ist ebenso wichtig: Der Boden muss für eine Verflüssigung gesättigt sein, daher sind Gebiete mit flachem Grundwasserspiegel (weniger als 5 Meter) am stärksten gefährdet. Aufgeschüttetes und zurückgewonnenes Land ist besonders anfällig, wie die Erdbeben von Niigata 1964 und Christchurch 2011 gezeigt haben.

Schlüsselfaktoren für das Verflüssigungsrisiko

Bodentyp: Lockere Sande und schluffige Sande sind am anfälligsten. Tone und Kiese widerstehen der Verflüssigung im Allgemeinen, obwohl nichtplastische Schluffe bei starken Erschütterungen verflüssigen können.
Grundwassertiefe: Flachere Grundwasserspiegel (0–5 m) erhöhen das Risiko dramatisch. Standorte mit Grundwasserspiegeln tiefer als 15 m sind im Allgemeinen vor Verflüssigung sicher.
Erschütterungsintensität und -dauer: Verflüssigung erfordert typischerweise anhaltende Erschütterungen (über mehrere Sekunden) bei Beschleunigungen über 0,1g. Länger andauernde Erdbeben erhöhen das Risiko.
Historischer Präzedenzfall: Gebiete, die bei vergangenen Erdbeben verflüssigt wurden, werden mit hoher Wahrscheinlichkeit erneut verflüssigen, da die geologischen Bedingungen, die Verflüssigung verursachen, bestehen bleiben.

Häufige Anwendungen

Vorläufige Bewertung des Verflüssigungspotenzials für die Immobilienbewertung in erdbebengefährdeten Küstengebieten.
Verstehen, welche Bodenverhältnisse und Erdbebenparameter zur Verflüssigung beitragen.
Bewertung des Risikos für Standorte auf Aufschüttungen, zurückgewonnenem Land oder in der Nähe von Flüssen und Küstenlinien.
Unterstützung pädagogischer Diskussionen über geotechnisches Erdbebeningenieurwesen.

How to Use

1
Enter Soil and Site Data
Input your site's soil type (sand, silt, clay, fill), water table depth, and layer thickness. Sandy soils saturated with water at depths less than 10 meters carry the highest liquefaction potential.
2
Specify the Earthquake Scenario
Enter the design earthquake magnitude (Mw) and peak ground acceleration (PGA) for your site. These can be obtained from the USGS seismic hazard map or from a site-specific hazard analysis at your return period of interest.
3
Interpret the Liquefaction Potential Index
Review your Liquefaction Potential Index (LPI) value and qualitative risk category. LPI < 5 is considered low risk; LPI 5–15 moderate; LPI > 15 high. The tool follows the Iwasaki (1982) framework widely used in Japanese and US engineering practice.

About

Soil liquefaction has been recognized as a major earthquake hazard since the 1964 Niigata and Alaska earthquakes, which produced dramatic documentary evidence of ground failure. The modern analytical framework for liquefaction assessment was developed largely by H. Bolton Seed and colleagues at UC Berkeley in the 1970s–80s, based on Standard Penetration Test (SPT) blow counts as a proxy for soil density and resistance. The Seed-Idriss Simplified Procedure, subsequently updated by Youd et al. (2001) and Idriss and Boulanger (2008), remains the standard for routine engineering practice and forms the basis of most liquefaction screening tools.

Liquefaction assessment methods fall into two categories. Deterministic methods compute a factor of safety for each soil layer using measured in-situ properties (SPT N-value, CPT qc, shear wave velocity Vs) and the earthquake loading expressed as the Cyclic Stress Ratio. Probabilistic methods (Cetin et al., 2004; Boulanger and Idriss, 2014) incorporate uncertainty in both the demand and capacity parameters to produce probability-of-liquefaction values rather than binary pass/fail outcomes. Probabilistic approaches are increasingly favored in performance-based earthquake engineering (PBEE) frameworks, where risk is expressed as expected losses over the lifetime of a facility.

The 2010–2011 Canterbury earthquake sequence in New Zealand produced an unprecedented dataset for liquefaction research. The earthquakes affected Christchurch—a city founded on Holocene fluvial sediments—causing liquefaction across 80% of the residential Red Zone, the area ultimately purchased by the government for permanent managed retreat. GNS Science and the University of Canterbury deployed a multi-technique investigation including aerial photography, LiDAR surveys, and thousands of CPT soundings to map spatial variability in liquefaction manifestation at block-by-block resolution. The resulting Christchurch Liquefaction Vulnerability dataset is now one of the most comprehensive post-earthquake geotechnical records ever assembled and has driven significant advances in simplified liquefaction assessment procedures.

FAQ

What is soil liquefaction?

Soil liquefaction is a phenomenon in which saturated, loosely packed granular sediment (typically sand or silt) temporarily loses its shear strength and behaves as a fluid when subjected to rapid cyclic loading such as earthquake shaking. The mechanism involves the buildup of excess pore water pressure: when the soil grains are rapidly jostled, the water between them cannot escape fast enough, and the pore pressure increases until it equals the confining stress, at which point the soil loses all effective stress and grain-to-grain contact. The soil-water mixture flows laterally under gravity, causing ground failure. Structures founded on liquefied soil can sink, tilt, or experience foundation failure even if they themselves are seismically well designed.

Welche Bodenarten sind am anfälligsten für Verflüssigung?

Liquefaction susceptibility is highest in saturated, loose to medium-dense clean sands and non-plastic silts with low plasticity (PI < 12), at depths less than 20 meters, with water table within 3 meters of the surface. The Chinese Criteria (Seed and Idriss, 1982) identified fine sands with fines content less than 15% as most vulnerable. Recent research has extended liquefaction risk to low-plasticity silts and some sensitive clays (the 'cyclic softening' mechanism). Poorly compacted fills—including hydraulic fills used to reclaim land—are particularly susceptible and are responsible for much liquefaction damage in New Zealand (2010–2011 Canterbury earthquakes), Japan (Tokyo Bay waterfront, 2011), and San Francisco (Marina District, 1989 Loma Prieta).

How does liquefaction damage buildings?

Liquefaction causes damage through several mechanisms. Sand boils (or sand volcanoes) form when pressurized pore water and sand erupt to the surface through cracks or utility penetrations. Differential settlement occurs when liquefied zones compact unevenly after pore pressure dissipates, tilting or cracking structures. Lateral spreading is perhaps the most destructive mechanism: when liquefied ground near a slope or riverbank flows laterally by meters to tens of meters, it ruptures pipelines, buckles roads, and moves building foundations. The 1964 Niigata earthquake caused entire apartment blocks to tilt 15–40 degrees through liquefaction-induced settlement; the 2011 Christchurch earthquake sequence caused NZ$1.5 billion in liquefaction-related building losses in residential areas.

Can liquefaction risk be reduced?

Liquefaction risk can be significantly reduced through ground improvement and structural mitigation techniques. Vibro-compaction and vibro-replacement (stone columns) densify loose granular soils in place or replace susceptible soils with dense aggregate columns. Dynamic compaction uses heavy tamper drops to densify surface layers. Deep soil mixing and jet grouting inject binders (cement or lime) to create strengthened columns or grids within susceptible zones. For new construction, mat foundations that 'float' on the soil, deep pile foundations extending through susceptible layers to bearing strata, and perimeter sheet pile walls to contain lateral spreading all reduce liquefaction vulnerability. For existing structures, perimeter soil treatment and underpinning with micropiles can retrofit foundation performance.

What is the Liquefaction Potential Index?

The Liquefaction Potential Index (LPI), proposed by Iwasaki et al. (1982) and widely adopted in Japanese seismic design practice, is a single-value parameter that integrates the factor of safety against liquefaction over the full soil profile to a depth of 20 meters. The factor of safety at each depth (FS = CRR/CSR) is computed from the Cyclic Resistance Ratio (CRR—the soil's capacity to resist liquefaction) and Cyclic Stress Ratio (CSR—the seismic demand). FS values less than 1.0 indicate liquefaction; these layers contribute most to the LPI with depth-weighting that emphasizes shallow soils. LPI ≤ 2 is considered very low risk; 2–5 low; 5–15 high; > 15 very high. The index correlates reasonably well with observed surface manifestations of liquefaction from earthquakes in Japan, New Zealand, and Taiwan.