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Introduction Modal Logic of Forcing Set-Theoretic Geology Some Second Order Set Theory Joel David Hamkins The City University of New York The College of Staten Island of CUNY The CUNY Graduate Center New York City Chennai, India January 2009 Second-order set theory, ICLA 2009 Joel David Hamkins, New York

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Introduction Modal Logic of Forcing Set-Theoretic Geology

Some Second Order Set Theory

Joel David Hamkins

The City University of New YorkThe College of Staten Island of CUNY

The CUNY Graduate CenterNew York City

Chennai, India January 2009

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

This talk includes a survey of collaborative work undertakenjointly with

Benedikt Löwe, Universiteit van Amsterdam, ILLC

Gunter Fuchs, Universität Münster

and

Jonas Reitz, New York City College of Technology.

Thanks to NWO Bezoekersbeurs for supporting my stays inAmsterdam 2005, 2006, 2007.

Thanks to National Science Foundation (USA) for supportingmy research 2008-2011.

Thanks to CUNY Research Foundation for supporting myresearch.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Set Theory

Set theory is the study of sets, particularly the transfinite, with afocus on well-founded transfinite recursion. Began with Cantorin late 19th century, matured in mid 20th century. Set theorytoday is vast: independence, large cardinals, forcing,combinatorics, the continuum, descriptive set theory,...

Set theory also serves as an ontological foundation for all (ormuch of) mathematics. Mathematical objects can be viewed ashaving a set theoretical essence. Natural numbers, rationals,reals, functions, topological spaces, etc. Mathematicalprecision often means specifying an object in set theory.

Set theory consequently speaks to or with other mathematicalsubjects, particularly on foundational matters.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Models of set theoryThe fundamental axioms of set theory are theZermelo-Fraenkel ZFC axioms, which concern set existence.

Each model of ZFC is an entire mathematical world, in whichany mathematician could be at home.

A mathematical statement ϕ can be proved independent of ZFCby providing a model of ZFC in which ϕ holds and another inwhich ϕ fails. For example, Gödel provided a model of ZFC inwhich the Continuum Hypothesis holds, and Cohen providedone in which it fails.

Set theorists have powerful methods to construct such models.e.g. forcing (Cohen 1963). We now have thousands.

As set theory has matured, the fundamental object of study hasbecome: the model of set theory.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Second order set theory

Set theory now exhibits a category-theoretic nature.

What we have is a vast cosmos of models of set theory, eachits own mathematical universe, connected by forcing extensionsand large cardinal embeddings.

The thesis of this talk is that, as a result, set theory nowexhibits an essential second-order nature.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Two emerging developmentsTwo emerging developments are focused on second-orderfeatures of the set theoretic universe.

Modal Logic of forcing. Upward-oriented, looking from amodel of set theory to its forcing extensions.

Set-theoretic geology. Downward-oriented, looking from amodel of set theory down to its ground models.

This analysis engages pleasantly with various philosophicalviews on the nature of mathematical existence.

In particular, the two perspectives are unified by and findmotivation in a multiverse view of set theory, the philosophicalview that there are many set-theoretic worlds.

I invite researchers to the topic. Many open questions remain.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Philosophy of mathematical existenceMathematical Platonism. Many set theorists hold that there isjust one universe of set theory, and our task is to understand it.

Paradoxically, however, the most powerful tools in set theoryare actually methods of constructing alternative universes. Webuild new models of set theory from existing models, via forcingand ultrapowers. These other models offer us glimpses ofalternative universes and alternative truths.

The Multiverse View. This philosophical position acceptsthese alternative universes as fully existing mathematically.

This is realism, not formalism, but rejects the uniqueness of themathematical universe. This philosophical view has guided theresearch on which I speak.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Forcing

Forcing (Cohen 1963) is a principal method of building modelsof set theory. It was used initially to prove the independence ofAxiom of Choice and the Continuum Hypothesis.

Subsequent explosion of applications: enormous variety ofmodels of set theory.

V ⊆ V [G]

The forcing extension V [G] is built from the ground model V byadding a new ideal object G.

The extension V [G] is closely related to the ground model V ,but exhibits new truths in a way that can be carefully controlled.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

How forcing worksSuppose V is a model of set theory, P a partial order in V .Suppose G ⊆ P is a V -generic filter, meaning that G ∩D 6= ∅ forall dense D ⊆ P in V .

The forcing extension V [G] adjoins G to V by closing underelementary set-building operations. Every object in V [G] has aname in V , and is built directly from its name and G.

p ϕ if every V -generic G with p ∈ G has V [G] |= ϕ.

Forcing Lemmas

1 The forcing extension V [G] satisfies ZFC.

2 If V [G] |= ϕ, then p ϕ for some p ∈ G.

3 The forcing relation p ϕ is definable in V .

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Affinity of Forcing & Modal Logic

This leads us naturally to the modal logic of forcing.

A ground model has access, via names and the forcing relation,to the objects and truths of the forcing extension.

So there is a natural Kripke model lurking here.

The possible worlds are the models of set theory.

The accessibility relation relates a model M to its forcingextensions M[G].

Many set theorists habitually operate within this Kripke model.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Modal operators

A sentence ϕ is possible or forceable, written ♦ϕ, when itholds in a forcing extension.

A sentence ϕ is necessary, written �ϕ, when it holds in allforcing extensions.

The modal assertions are expressible in set theory:

♦ϕ ↔ ∃P P ϕ

�ϕ ↔ ∀P P ϕ

While ♦ and � are eliminable, we nevertheless retain themhere, because we are interested in what principles theseoperators must obey.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Easy forcing validitiesK �(ϕ→ ψ) → (�ϕ→ �ψ)Dual �¬ϕ↔ ¬♦ϕS �ϕ→ ϕ4 �ϕ→ ��ϕ.2 ♦�ϕ→ �♦ϕ

Theorem

Any S4.2 modal assertion is a valid principle of forcing.

ϕ(p0, . . . ,pn) is a valid principle of forcing if ϕ(ψ0, . . . , ψn) holdsfor any set theoretical ψi .

Q

What are the valid principles of forcing?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Easy forcing validitiesK �(ϕ→ ψ) → (�ϕ→ �ψ)Dual �¬ϕ↔ ¬♦ϕS �ϕ→ ϕ4 �ϕ→ ��ϕ.2 ♦�ϕ→ �♦ϕ

Theorem

Any S4.2 modal assertion is a valid principle of forcing.

ϕ(p0, . . . ,pn) is a valid principle of forcing if ϕ(ψ0, . . . , ψn) holdsfor any set theoretical ψi .

Q

What are the valid principles of forcing?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Easy forcing validitiesK �(ϕ→ ψ) → (�ϕ→ �ψ)Dual �¬ϕ↔ ¬♦ϕS �ϕ→ ϕ4 �ϕ→ ��ϕ.2 ♦�ϕ→ �♦ϕ

Theorem

Any S4.2 modal assertion is a valid principle of forcing.

ϕ(p0, . . . ,pn) is a valid principle of forcing if ϕ(ψ0, . . . , ψn) holdsfor any set theoretical ψi .

Q

What are the valid principles of forcing?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Beyond S4.2

5 ♦�ϕ→ ϕM �♦ϕ→ ♦�ϕ

W5 ♦�ϕ→ (ϕ→ �ϕ).3 ♦ϕ ∧ ♦ψ → (♦(ϕ ∧ ♦ψ) ∨ ♦(ϕ ∧ ψ) ∨ ♦(ψ ∧ ♦ϕ))

Dm �(�(ϕ→ �ϕ) → ϕ) → (♦�ϕ→ ϕ)Grz �(�(ϕ→ �ϕ) → ϕ) → ϕLöb �(�ϕ→ ϕ) → �ϕ

H ϕ→ �(♦ϕ→ ϕ)

It is a fun forcing exercise to show that these are invalid in some or allmodels of ZFC. Counterexamples built from such assertions asV 6= L, ωL

1 < ω1, CH, or Boolean combinations of these.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Affinity of Forcing & Modal Logic

Some common modal theories

S5 = S4 + 5S4W5 = S4 + W5

S4.3 = S4 + .3S4.2.1 = S4 + .2 + M

S4.2 = S4 + .2S4.1 = S4 + M

S4 = K4 + SDm.2 = S4.2 + Dm

Dm = S4 + DmGrz = K + GrzGL = K4 + Löb

K4H = K4 + HK4 = K + 4

K = K + Dual

S5

S4W5?

S4.2.1 S4.3?

Dm.2

-Grz

S4.1?

S4.2?�

-Dm?�

K4H

GL

S4?�

-

K4?�

-

K?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Valid principles of forcing

Theorem (Hamkins,Löwe)

If ZFC is consistent, then the ZFC-provably valid principles offorcing are exactly S4.2.

We know S4.2 is valid. The difficult part is to show that nothingelse is valid.

Given S4.2 6` ϕ, we must provide ψi such that ϕ(ψ0, . . . , ψn)fails in some model of set theory.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Buttons and Switches

A switch is a statement ϕ such that both ϕ and ¬ϕ arenecessarily possible.

A button is a statement ϕ such that ϕ is (necessarily)possibly necessary.

Fact. Every statement in set theory is either a switch, a buttonor the negation of a button.

Theorem

If V = L, then there is an infinite independent family of buttonsand switches.

Buttons: bn = “ ℵLn is collapsed ”

Switches: sm = “ GCH holds at ℵω+m ”

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Kripke models and framesKripke models provide a general modal semantics. A Kripkemodel is a collection of propositional worlds, with an underlyingaccessibility relation called the frame.

Partial pre-order implies S4. Directed pre-order implies S4.2

Fact

If S4.2 6` ϕ, then ϕ fails in a Kripke model whose frame is afinite directed partial pre-order.

Improved Fact

If S4.2 6` ϕ, then ϕ fails in a Kripke model whose frame is afinite pre-lattice.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Simulating Kripke models

Lemma

If W |= ZFC has buttons and switches, then for any Kripkemodel M on a finite pre-lattice frame, any w ∈ M, there ispi 7→ ψi so that for any ϕ:

(M,w) |= ϕ(p1, . . . ,pn) ↔ W |= ϕ(ψ1, . . . , ψn).

Consequently, if S4.2 6` ϕ, then there is a substitution instancesuch that W |= ¬ϕ(ψ1, . . . , ψn).

Main Theorem

If ZFC is consistent, then the ZFC-provable forcing validities areexactly S4.2.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Simulating Kripke models

Lemma

If W |= ZFC has buttons and switches, then for any Kripkemodel M on a finite pre-lattice frame, any w ∈ M, there ispi 7→ ψi so that for any ϕ:

(M,w) |= ϕ(p1, . . . ,pn) ↔ W |= ϕ(ψ1, . . . , ψn).

Consequently, if S4.2 6` ϕ, then there is a substitution instancesuch that W |= ¬ϕ(ψ1, . . . , ψn).

Main Theorem

If ZFC is consistent, then the ZFC-provable forcing validities areexactly S4.2.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Simulating Kripke models

Lemma

If W |= ZFC has buttons and switches, then for any Kripkemodel M on a finite pre-lattice frame, any w ∈ M, there ispi 7→ ψi so that for any ϕ:

(M,w) |= ϕ(p1, . . . ,pn) ↔ W |= ϕ(ψ1, . . . , ψn).

Consequently, if S4.2 6` ϕ, then there is a substitution instancesuch that W |= ¬ϕ(ψ1, . . . , ψn).

Main Theorem

If ZFC is consistent, then the ZFC-provable forcing validities areexactly S4.2.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Validities in a modelFor W |= ZFC, let ϕ ∈ ForceW if ϕ is valid for forcing over W .

Theorem

S4.2 ⊆ ForceW ⊆ S5.

Both endpoints occur for various W .

Question

Can we have S4.2 ( ForceW ( S5?

Question

If ϕ is valid for forcing over W , does it remain valid for forcingover all extensions of W? Equivalently, is ForceW normal?

Question

Can a model of ZFC have an unpushed button, but not twoindependent buttons?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Surprising entry of large cardinals

Theorem. The following are equiconsistent:

1 S5(R) is valid.

2 S4W5(R) is valid for forcing.

3 Dm(R) is valid for forcing.

4 There is a stationary proper class of inaccessible cardinals.

Theorem

1 (Welch,Woodin) If S5(R) is valid in all forcing extensions(using R of extension), then ADL(R).

2 (Woodin) If ADR + Θ is regular, then it is consistent thatS5(R) is valid in all extensions.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Valid Principles of Forcing

Topics of current research

Investigate validities of a model W |= ZFC.

What is the modal logic of ccc forcing? proper forcing? etc.

What is the modal logic of class forcing, or of arbitrary ZFCextensions?

Leads to: the set theoretical multiverse.

Modal logic of the corresponding downwards operator.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

A new perspectiveForcing is naturally viewed as a method of building outer asopposed to inner models of set theory.

Nevertheless, a simple switch in perspective allows us to viewforcing as a method of producing inner models as well.

Namely, we look for how the universe V might itself have arisenvia forcing. Given V , we look for classes W ⊆ V of which theuniverse V is a forcing extension by some W -generic filterG ⊆ P ∈ W

W ⊆ W [G] = V

This change in viewpoint results in the subject we callset-theoretic geology. Many open questions remain. Here, Igive a few of the most attractive initial results...

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

A new perspectiveForcing is naturally viewed as a method of building outer asopposed to inner models of set theory.

Nevertheless, a simple switch in perspective allows us to viewforcing as a method of producing inner models as well.

Namely, we look for how the universe V might itself have arisenvia forcing. Given V , we look for classes W ⊆ V of which theuniverse V is a forcing extension by some W -generic filterG ⊆ P ∈ W

W ⊆ W [G] = V

This change in viewpoint results in the subject we callset-theoretic geology. Many open questions remain. Here, Igive a few of the most attractive initial results...

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

Digging for GroundsA transitive class W is a ground of the universe V if it is amodel of ZFC over which V is obtained by set forcing, that is, ifthere is some forcing notion P ∈ W and a W -generic filterG ⊆ P such that V = W [G].

Theorem (Laver, independently Woodin)

Every ground W is a definable class in its forcing extensionsW [G], using parameters in W.

Laver’s proof used my methods on approximation and covering.

Definition (Hamkins,Reitz)

The Ground Axiom is the assertion that the universe V has nonontrivial grounds.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

The Ground Axiom is first orderThe Ground Axiom GA asserts that the universe was notobtained by set forcing over an inner model.

At first, this appears to be a second order assertion, because itquantifies over grounds. But:

Theorem (Reitz)

The Ground Axiom is first order expressible in set theory.

The Ground Axiom holds in many canonical models of settheory: L, L[0]], L[µ], many instances of K .

Question: To what extent are the highly regular features ofthese models consequences of GA?

Answer: Not at all.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

The Ground Axiom is first orderThe Ground Axiom GA asserts that the universe was notobtained by set forcing over an inner model.

At first, this appears to be a second order assertion, because itquantifies over grounds. But:

Theorem (Reitz)

The Ground Axiom is first order expressible in set theory.

The Ground Axiom holds in many canonical models of settheory: L, L[0]], L[µ], many instances of K .

Question: To what extent are the highly regular features ofthese models consequences of GA?

Answer: Not at all.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

Consequences of the Ground AxiomTheorem (Reitz)

Every model of ZFC has an extension, preserving any desiredVα, which is a model of GA.

Thus, the Ground Axiom does not imply any of the usualcombinatorial set-theoretic regularity features ♦, GCH, etc.

What about V = HOD? Reitz’s method obtains GA by forcingvery strong versions of V = HOD.

Theorem (Hamkins,Reitz,Woodin)

Every model of set theory has an extension which is a model ofGA plus V 6= HOD.

Preparatory forcing, followed by Silver iteration. Very robust.Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

Consequences of the Ground AxiomTheorem (Reitz)

Every model of ZFC has an extension, preserving any desiredVα, which is a model of GA.

Thus, the Ground Axiom does not imply any of the usualcombinatorial set-theoretic regularity features ♦, GCH, etc.

What about V = HOD? Reitz’s method obtains GA by forcingvery strong versions of V = HOD.

Theorem (Hamkins,Reitz,Woodin)

Every model of set theory has an extension which is a model ofGA plus V 6= HOD.

Preparatory forcing, followed by Silver iteration. Very robust.Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

BedrocksW is a bedrock of V if it is a ground of V and minimal withrespect to the forcing extension relation.

Equivalently, W is a bedrock of V if it is a ground of V andsatisfies GA.

Open Question

Is the bedrock unique when it exists?

Theorem (Reitz)

It is relatively consistent with ZFC that the universe V has nobedrock model.

Such models are bottomless.Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

The MantleWe now carry the investigation deeper underground.

The principal new concept is the Mantle.

Definition

The Mantle M is the intersection of all grounds.

The analysis engages with an interesting philosophical view:

Ancient Paradise. This is the philosophical view that there is ahighly regular core underlying the universe of set theory, aninner model obscured over the eons by the accumulating layersof debris heaped up by innumerable forcing constructions sincethe beginning of time. If we could sweep the accumulatedmaterial away, we should find an ancient paradise.

The Mantle, of course, wipes away an entire strata of forcing.Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

The MantleWe now carry the investigation deeper underground.

The principal new concept is the Mantle.

Definition

The Mantle M is the intersection of all grounds.

The analysis engages with an interesting philosophical view:

Ancient Paradise. This is the philosophical view that there is ahighly regular core underlying the universe of set theory, aninner model obscured over the eons by the accumulating layersof debris heaped up by innumerable forcing constructions sincethe beginning of time. If we could sweep the accumulatedmaterial away, we should find an ancient paradise.

The Mantle, of course, wipes away an entire strata of forcing.Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Grounds, Bedrocks, the Mantle

Every model is a mantle

Although that philosophical view is highly appealing, our maintheorem tends to refute it.

Main Theorem

Every model of ZFC is the mantle of another model of ZFC.

By sweeping away the accumulated sands of forcing, what wefind is not a highly regular ancient core, but rather: an arbitrarymodel of set theory.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The grounds form a parameterized family

Theorem

There is a parameterized family {Wr | r ∈ V } of classes suchthat

1 Every Wr is a ground of V and r ∈ Wr .

2 Every ground of V is Wr for some r.

3 The relation “x ∈ Wr ” is first order.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

Reducing Second to First order

The parameterized family {Wr | r ∈ V } of grounds reduces2nd order properties about grounds to 1st order propertiesabout parameters.

The Ground Axiom holds if and only if ∀r Wr = V .

Wr is a bedrock if and only if ∀s (Ws ⊆ Wr → Ws = Wr ).

The Mantle is defined by M = { x | ∀r (x ∈ Wr ) }.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

Downward directedness

Definition

1 The grounds are downward directed if for every r and sthere is t such that Wt ⊆ Wr ∩Ws.

2 They are locally downward directed if for every B and everyr , s there is t with Wt ∩ B ⊆ Wr ∩Ws.

Question (Reitz)

Is the bedrock unique when it exists? Are the groundsdownward directed?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

Downward set-directedness

Definition

1 The grounds are downward set-directed if for every A thereis t with Wt ⊆

⋂r∈A Wr .

2 They are locally downward set-directed if for every A,Bthere is t with Wt ∩ B ⊆

⋂r∈A Wr .

Open question

Are the grounds downward set directed?

In every model for which we can determine the answer, theanswer is yes.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Mantle under directedness

If the grounds are downward directed, the Mantle is wellbehaved.

Theorem

1 If the grounds are downward directed, then the Mantle isconstant across the grounds, and M |= ZF.

2 If they are downward set-directed, then M |= ZFC.

We actually only need downward directed plus locallydownward set-directed in (2).

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic Mantle

We defined the Mantle to be the intersection of all grounds of V .

Let the Generic Mantle, denoted gM, be the intersection of allgrounds of all forcing extensions of V .

Any ground of V is a ground of any forcing extension of V , sothe generic Mantle is the intersection of more models.

Thus, gM ⊆ M.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The generic multiverse

The Generic Multiverse is the family of universes obtained byclosing under forcing extensions and grounds.

There are various philosophical motivations to study thegeneric multiverse.

Woodin introduced the generic multiverse essentially to rejectit, to defeat a certain multiverse view of truth.

Our view is that the generic multiverse is a natural context forset-theoretic investigation, and it should be a principal focus ofstudy.

A multiverse path is 〈U0, . . . ,Un〉, where each Ui+1 is either aground or forcing extension of Ui .

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The generic multiverse

The Generic Multiverse is the family of universes obtained byclosing under forcing extensions and grounds.

There are various philosophical motivations to study thegeneric multiverse.

Woodin introduced the generic multiverse essentially to rejectit, to defeat a certain multiverse view of truth.

Our view is that the generic multiverse is a natural context forset-theoretic investigation, and it should be a principal focus ofstudy.

A multiverse path is 〈U0, . . . ,Un〉, where each Ui+1 is either aground or forcing extension of Ui .

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The generic multiverse

The Generic Multiverse is the family of universes obtained byclosing under forcing extensions and grounds.

There are various philosophical motivations to study thegeneric multiverse.

Woodin introduced the generic multiverse essentially to rejectit, to defeat a certain multiverse view of truth.

Our view is that the generic multiverse is a natural context forset-theoretic investigation, and it should be a principal focus ofstudy.

A multiverse path is 〈U0, . . . ,Un〉, where each Ui+1 is either aground or forcing extension of Ui .

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic Mantle

Theorem

The generic Mantle gM is a parameter-free uniformly definableclass, invariant by forcing, containing all ordinals and gM |= ZF.

Since the generic Mantle is invariant by forcing, it follows that:

Corollary

The generic Mantle gM is constant across the multiverse. Infact, gM is the intersection of the generic multiverse.

On this view, the generic Mantle is a canonical, fundamentalfeature of the generic multiverse, deserving of intense study.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic Mantle

Theorem

The generic Mantle gM is a parameter-free uniformly definableclass, invariant by forcing, containing all ordinals and gM |= ZF.

Since the generic Mantle is invariant by forcing, it follows that:

Corollary

The generic Mantle gM is constant across the multiverse. Infact, gM is the intersection of the generic multiverse.

On this view, the generic Mantle is a canonical, fundamentalfeature of the generic multiverse, deserving of intense study.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

Grounds and generic Grounds

Theorem

If the generic grounds are downward directed, then the groundsare dense below the generic multiverse, and so M = gM.

In this case, the generic multiverse is exhausted by the groundextensions Wr [G]. (So multiverse paths of length 2 suffice.)

Observation

It is relatively consistent that the generic grounds do notexhaust the generic multiverse.

Proof.

If V [c] and V [d ] are not amalgamable, then V [d ] is not ageneric ground of V [c], but they have the same multiverse.

Theorem

If the generic grounds are locally downward set-directed, thengM |= ZFC.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic HOD

HOD is the class of hereditarily ordinal definable sets.

HOD |= ZFC

The generic HOD, introduced by Fuchs, is the intersection of allHODs of all forcing extensions.

gHOD =⋂G

HODV [G]

The original motivation was to identify a very large canonicalforcing invariant class.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic HOD

HOD is the class of hereditarily ordinal definable sets.

HOD |= ZFC

The generic HOD, introduced by Fuchs, is the intersection of allHODs of all forcing extensions.

gHOD =⋂G

HODV [G]

The original motivation was to identify a very large canonicalforcing invariant class.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

The Mantle, directedness, generic Mantle, generic HOD

The Generic HOD

Facts

1 gHOD is constant across the generic multiverse.

2 The HODs of all forcing extensions are downwardset-directed.

3 Consequently, gHOD is locally realized and gHOD |= ZFC.

4 The following inclusions hold.

HOD

gHOD ⊆ gM ⊆ M

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Separating the notions

HOD

gHOD ⊆ gM ⊆ M

To what extent can we control and separate these classes?

We answer with our main theorems.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

First Main Theorem

First, we can control the classes to keep them all low.

Main Theorem

If V |= ZFC, then there is a class extension V [G] in which

V = MV [G] = gMV [G] = gHODV [G] = HODV [G]

In particular, as mentioned earlier, every model of ZFC is themantle and generic mantle of another model of ZFC.

It follows that we cannot expect to prove ANY regularityfeatures about the mantle or the generic mantle.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Proof ideas

The initial idea goes back to McAloon (1971), to make setsdefinable by forcing.

For an easy case, consider an arbitrary real x ⊆ ω. It may nothappen to be definable in V .

With an infinite product, we can force the GCH to hold at ℵn

exactly when x(n) = 1.

In the resulting forcing extension V [G], the original real x isdefinable, without parameters.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Proof sketchFor the main theorem, start in V |= ZFC. Want V [G] withV = MV [G] = gMV [G] = gHODV [G] = HODV [G].

Let Qα generically decide whether to force GCH or ¬GCH at ℵα (*).Let P = ΠαQα, with set support. Consider V [G] for generic G ⊆ P.

Every set in V becomes coded unboundedly into the continuumfunction of V [G]. Hence, definable in V [G] and all extensions.

So V ⊆ gHOD. Consequently V ⊆ gHOD⊆ gM ⊆ M and V ⊆ HOD.

Every tail segment V [Gα] is a ground of V [G]. Also, ∩αV [Gα] = V .Thus, M ⊆ V . Consequently, V = gHOD = gM = M.

HODV [G] ⊆ HODV [Gα], since P � α is densely almost homogeneous.

So HODV [G] ⊆ V .

In summary, V = MV [G] = gMV [G] = gHODV [G] = HODV [G], as desired.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Second Main Theorem: Mantles low, HOD high

Main Theorem 2

If V |= ZFC, then there is a class extension V [G] in which

V = MV [G] = gMV [G] = gHODV [G] but HODV [G] = V [G]

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Proof ideasWant an extension V [G] with

V = MV [G] = gMV [G] = gHODV [G] but HODV [G] = V [G]

Balance the forces on M, gM, gHOD and HOD.

Force to V [G] where every set in V is coded unboundedlyin the GCH pattern.

Also ensure that G is definable, but not robustly.

The proof uses self-encoding forcing:

Add a subset A ⊆ κ. Then code this set A into theGCH pattern above κ. Then code THOSE setsinto the GCH pattern, etc. Get extension V [G(κ)]in which G(κ) is definable.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Keeping HODs low, Mantles highNext, we keep the HODs low and the Mantles high, seekingV [G] with V = HODV [G] = gHODV [G] but MV [G] = V [G].

Such a model V [G] will of course be a model of the GroundAxiom plus V 6= HOD. Recall

Theorem (Hamkins,Reitz,Woodin)

Every V |= ZFC has a class forcing extensionV [G] |= GA + V 6= HOD.

We modified the argument to obtain:

Theorem

If V |= ZFC, then there is a class extension V [G] in which

V = HODV [G] = gHODV [G] but MV [G] = V [G]

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Mantles high, HODs high

Lastly,

Theorem

If V |= ZFC, then there is V [G] in which

V [G] = HODV [G] = gHODV [G] = MV [G] = gMV [G]

This is possible by forcing the Continuum Coding Axiom CCA.

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

The Inner Mantles

When the Mantle M is a model of ZFC, we may consider theMantle of the Mantle, iterating to reveal the inner Mantles:

M1 = M Mα+1 = MMαMλ =

⋂α<λ

Continue as long as the model satisfies ZFC.

The Outer Core is reached if Mα has no grounds,Mα |= ZFC+ GA.

Conjecture. Every model of ZFC is the αth inner Mantle ofanother model, for arbitrary α ≤ ORD.

Philosophical view: ancient paradise?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Questions

Set-theoretic geology is a young area, and there are a largenumber of open questions.

To what extent does the Mantle satisfy ZF or ZFC?

Are the grounds or generic grounds downward directed?downward set-directed? locally?

Is the bedrock unique when it exists?

Is gM = M? Is gM = gHOD?

Does the generic Mantle satisfy ZFC?

Second-order set theory, ICLA 2009 Joel David Hamkins, New York

Introduction Modal Logic of Forcing Set-Theoretic Geology

Controlling the Mantle

Thank you.

Joel David HamkinsThe City University of New York

http://jdh.hamkins.org

Second-order set theory, ICLA 2009 Joel David Hamkins, New York