Sławatycze · ice from an oxbow lake of the Bug

Winter hidden in a cross-section

July on one side, January on the other, and a layer of sawdust between them. This cross-section separates three things that are easy to confuse in the story of an icehouse: heat from outside, insulation, and water that drains away or stays put.

Small drawing locating the cross-section Schematic stack in the shape of a truncated pyramid: an outer layer of sawdust with a core of ice inside. A dashed arrow runs from the outside through the sawdust to the core and marks the line of the cross-section shown alongside.
Where the cross-section runs. General shape, described as a ‘pyramid’; not a plan of an icehouse.

July · air

Outside

Heat presses on the surface of the stack. In the model it is a single number Q, not a temperature in degrees.

Q is the heat input in conventional units from 0 to 100. It is not the weather in Sławatycze or a measurement; it serves only to compare two covers.

Insulation

Sawdust

They reduce how much heat reaches the ice. In the model: parameter S.

The description of the tradition says that the stack was covered with sawdust. Why sawdust insulates: it is porous, and still air in the voids conducts heat poorly. This is a general explanation, not a measurement from Sławatycze.

The thickness of the layer and the kind of sawdust are not given in the material supplied: no data, not zero.

January sealed in the stack

Inside

A compact stack of ice slabs. In the model it starts with 100 units of ice.

According to the description, slabs were harvested in winter from an oxbow lake of the Bug and laid in a large stack called a pyramid. The drawing is general: the number and size of the slabs and the local construction are not established.

Ground (schematic)

Meltwater drainage · this is not insulation

Drainage does not change how much ice melts. It only decides whether the water lies in the store or outside it.

The description of the tradition supplied says nothing about water draining from the stack in Sławatycze: it is an element of the diagram, not a fact about that place.

In the model, water does not speed up melting. In a real store, standing water could change the heat exchange; we do not calculate that here.

DIAGRAM · not to scaleAn explanatory montage that sets two seasons side by side. It is not a photograph or a plan of a historical icehouse. Colours and textures are conventional. For each layer, the description opens beneath its button.

Take off a layer · teaching model

The cover changes how much ice is left. Drainage only changes where the water lies.

Every bar below is the same 100 conventional units. The two rows have different covers, the two columns different drainage, and the heat Q is shared. Take the cover off variant B and compare the rows, then glance at the columns: the ice changes only between rows.

Rules of the model (always the same):

  1. Melted = Q × (1 − S), no more than 100 units.
  2. Ice = 100 − melted.
  3. Melted water lies in the store or is drained out of it. Ice + water in the store + water outside the store = 100.
0 = no input, 100 = upper limit of the model scale.

Ice difference A − B+30 units

Without JavaScript you see example values: Q = 60, cover A = 70%, cover B = 20%. The sliders require JavaScript.

Ice Water lying in the store Water drained outside the store (dashed line = store boundary)

Variant A

Drainage: yes

Ice
82 units
Water in the store
0 units
Water outside the store
18 units
Total
100 units

Drainage: no

Ice
82 units
Water in the store
18 units
Water outside the store
0 units
Total
100 units

Variant B

Drainage: yes

Ice
52 units
Water in the store
0 units
Water outside the store
48 units
Total
100 units

Drainage: no

Ice
52 units
Water in the store
48 units
Water outside the store
0 units
Total
100 units
+30 units

Variant A (cover 70%) keeps 30 units more ice than variant B (cover 20%): 82 versus 52 at Q = 60. Changing the drainage in the same row does not change the ice; it moves water between ‘lies in the store’ and ‘outside the store’.

Assumptions: initial mass 100 units, S in the range 0–90% (a cover does not insulate one hundred per cent), Q in the range 0–100. Drainage does not affect the rate of melting. The result illustrates a relationship; it is not a forecast of the fate of any real stack.

The evidence and its limits

Winter transport. Summer need.

According to the description of Lody sławatyckie [Sławatycze ice cream] on the List of Traditional Products, ice was harvested in winter from an oxbow lake of the Bug, carried on carts, laid in a large stack described as a pyramid and covered with sawdust with summer in mind, when it was needed to make traditional ice cream.

  1. Winter: harvesting slabs from the oxbow lake
  2. Winter: carrying them on carts
  3. A pyramid-shaped stack
  4. Covering with sawdust
  5. Summer: ice for making ice cream

This description was carried over from the previous version of the page; the source was not reopened at this stage, so it needs to be checked again. It describes a custom, not the design of an icehouse or the fate of a single block. It contains no loss curve, so a rate of melting cannot be calculated from it.

Melting changes the state of matter; it does not destroy mass: ice becomes water. That is why the total in the model is always 100.

Safety. The description of this former work is not an instruction and does not say when ice is safe. Natural ice on a river or oxbow lake can be unpredictable: do not walk on it. The page does not encourage cutting ice today.
What is a fact from the evidence and what is an assumption of the model
From the evidenceIn the model
Slabs in winter from an oxbow lake of the Bug100 conventional units of ice at the start
Stack described as a pyramidGeneral cross-section through the stack
Covering with sawdustParameter S: 0–90% reduction of heat input
Water drainage: no dataThe drainage switch decides only where the water is
Thickness of sawdust, dimensions of the stack, rate of melting: no dataQ is a conventional number; the model does not give a date of melting

Sources and caveats

Sources and limits

Links

  1. Lody sławatyckie – MRiRW, Lista Produktów Tradycyjnych [Sławatycze ice cream – Ministry of Agriculture and Rural Development, List of Traditional Products] Basis for the sentence about the oxbow lake of the Bug, carts, the pyramid and sawdust. Link carried over from the previous version; not opened at this stage, needs checking.
  2. Stany skupienia materii – ZPE [States of matter – ZPE] Basis for the remark that melting changes the state of matter. Link carried over from the previous version; not opened at this stage, needs checking.
  3. Wikimedia Commons: ice elevator, USA, 1914 (public domain mark) Comparative material, not Sławatycze or the Bug. The photograph is not embedded on the page, only linked; rights status as in the previous version, to be checked.

Limits and changes relative to V2

  • The drawing is the author’s own diagram, not a map or a plan. Colours and textures are conventional.
  • The model’s units are conventional; Q is not a temperature, and the result is not a forecast for Sławatycze.
  • The separate calculator with an initial mass and saving in the browser have been removed: two rows and a shared Q cover the same formulas, and nothing here requires data to be saved.
  • A 2×2 matrix replaced two independent sets of sliders, because it shows side by side that the cover and the drainage act on different quantities.
  • A link replaced the photograph from an external server so that the page works offline.
  • The target addresses of the catalogue, V1 and V2, and the external sources have not been checked here.