-
Notifications
You must be signed in to change notification settings - Fork 0
/
Copy pathhr_05_physical_properties.qmd
518 lines (395 loc) · 26.1 KB
/
hr_05_physical_properties.qmd
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
23
24
25
26
27
28
29
30
31
32
33
34
35
36
37
38
39
40
41
42
43
44
45
46
47
48
49
50
51
52
53
54
55
56
57
58
59
60
61
62
63
64
65
66
67
68
69
70
71
72
73
74
75
76
77
78
79
80
81
82
83
84
85
86
87
88
89
90
91
92
93
94
95
96
97
98
99
100
101
102
103
104
105
106
107
108
109
110
111
112
113
114
115
116
117
118
119
120
121
122
123
124
125
126
127
128
129
130
131
132
133
134
135
136
137
138
139
140
141
142
143
144
145
146
147
148
149
150
151
152
153
154
155
156
157
158
159
160
161
162
163
164
165
166
167
168
169
170
171
172
173
174
175
176
177
178
179
180
181
182
183
184
185
186
187
188
189
190
191
192
193
194
195
196
197
198
199
200
201
202
203
204
205
206
207
208
209
210
211
212
213
214
215
216
217
218
219
220
221
222
223
224
225
226
227
228
229
230
231
232
233
234
235
236
237
238
239
240
241
242
243
244
245
246
247
248
249
250
251
252
253
254
255
256
257
258
259
260
261
262
263
264
265
266
267
268
269
270
271
272
273
274
275
276
277
278
279
280
281
282
283
284
285
286
287
288
289
290
291
292
293
294
295
296
297
298
299
300
301
302
303
304
305
306
307
308
309
310
311
312
313
314
315
316
317
318
319
320
321
322
323
324
325
326
327
328
329
330
331
332
333
334
335
336
337
338
339
340
341
342
343
344
345
346
347
348
349
350
351
352
353
354
355
356
357
358
359
360
361
362
363
364
365
366
367
368
369
370
371
372
373
374
375
376
377
378
379
380
381
382
383
384
385
386
387
388
389
390
391
392
393
394
395
396
397
398
399
400
401
402
403
404
405
406
407
408
409
410
411
412
413
414
415
416
417
418
419
420
421
422
423
424
425
426
427
428
429
430
431
432
433
434
435
436
437
438
439
440
441
442
443
444
445
446
447
448
449
450
451
452
453
454
455
456
457
458
459
460
461
462
463
464
465
466
467
468
469
470
471
472
473
474
475
476
477
478
479
480
481
482
483
484
485
486
487
488
489
490
491
492
493
494
495
496
497
498
499
500
501
502
503
504
505
506
507
508
509
510
511
512
513
514
515
516
517
518
---
output: html_document
editor_options:
chunk_output_type: console
---
# Consistence {#sec-cons}
```{r}
library(dplyr)
library(tibble)
library(gt)
library(gtExtras)
```
[Consistence is a general term for the field-assessed behaviour of soil materials in response to applied stress over a range of soil-water states from wet to dry. The consistence properties described are strength, failure, fluidity, penetration resistance, packing, sensitivity, induration, plasticity, stickiness, dilatancy, and dry coherence.]{.milne}
Consistency tests should be performed down-profile, with at least one sample tested per horizon. Samples should be taken from the mid-point of each horizon. Additional samples in transition zones may also be of interest.
::: {#nte-consnzsc .callout-note appearance="minimal" collapse="true" title="Consistence tests and the New Zealand Soil Classification (NZSC)"}
For classifying using the NZSC, particular tests down to a certain depth may be required. At the order level:
- **Gley soils:** must not have any moderately or very fluid (@sec-cn-flu) layers within 30 cm of the soil surface. Unconfined soil strength (@sec-cn-stru) and cementation (@sec-cn-ind) tests may be required to confirm absence of an underlying fragipan.
- **Ultic soils:** need an assessment of soil strength (@sec-cn-stru) in the B horizon under moist conditions. May need assessment of failure mode (@sec-cn-fail) over a range of moisture conditions to rule out oxidic or cutanoxidic horizons. May need assessment of sensitivity (@sec-cn-sens) and stickiness (@sec-cn-sti) to rule out allophanic soil materials.
- **Podzols:** may need unconfined strength (@sec-cn-stru) and failure mode (@sec-cn-fail) tests to help identify a Podzolic B horizon, as well as the presence of humus- and ortstein-pans.
- **Allophanic soils:** may need assessment of sensitivity (@sec-cn-sens) and stickiness (@sec-cn-sti) to help confirm allophanic soil materials.
- **Melanic soils:** may require stickiness assessment (@sec-cn-sti) in the B horizon.
- **Semiarid soils:** may require cementation tests (@sec-cn-ind) to confirm fragipan absence.
- **Oxidic soils:** May need assessment of ped strength (@sec-cn-stra), soil strength (@sec-cn-stru), and failure mode (@sec-cn-fail) over a range of moisture conditions to confirm presence of an oxidic horizon. Stickiness (@sec-cn-sti) and plasticity (@sec-cn-pla) may also be helpful.
- **Granular soils:** May need assessment of ped strength (@sec-cn-stra), soil strength (@sec-cn-stru), and failure mode (@sec-cn-fail) over a range of moisture conditions to confirm presence of a cutanoxidic horizon. Stickiness (@sec-cn-sti) and plasticity (@sec-cn-pla) may also be helpful.
- **Pallic soils:** may require cementation tests (@sec-cn-ind) to confirm fragipan presence. May require assessment of failure mode (@sec-cn-fail) to help confirm Brittle-B horizon presence. May require ped strength assessment in the B horizon.
- **Recent soils:** must not have any moderately or very fluid (@sec-cn-flu) layers within 30 cm of the soil surface.
:::
## Preparing for consistence assessment {#sec-dn-prep}
[The nature of the soil materials in each horizon determines what tests can and should be done. The first step is to determine if the sample is cohesive.]{.milne}
- [**Cohesive soil materials** may have plasticity and stickiness characteristics and have a strength which can be measured in unconfined compression. All listed properties, except particle packing, can be described for non-gravelly, cohesive soils.]{.milne}
- [**Non-cohesive soil materials** have no shear resistance other than that developed by internal friction between grains. Non-cohesive soil materials, by definition, have no unconfined dry strength or plasticity, and the only property that can be meaningfully described is degree of packing or particle packing.]{.milne}
[The range of properties which can be described in gravelly, cohesive soils varies with gravel content. In practice, this depends on the feasibility of obtaining samples for the required tests.]{.milne}
[The distinction between cohesive and non-cohesive is recognised by performing moulding, plasticity, and dilatancy tests in the following sequence (@fig-cn-cohes).]{.milne} Where doubt still remains after these tests have been completed, the dry coherence test (@sec-cn-dryco) may be necessary.
```{mermaid}
%%| label: fig-cn-cohes
%%| fig-cap: Determining sample cohesion
flowchart TD
q1["Can a sample cube be formed from remoulded material?"] -->|yes| q2["Is the material plastic?"]
q2 ---->|yes| a1(["**Cohesive**"])
q1 -->|no| q3["Is the material plastic?"]
q3 -->|yes| q4
q2 -->|no| q4["Does the material have a fast positive reaction to the dilatency test?"]
q4 -->|no| q5["Does the material have a distinctly negative reaction to the dilatency test?"]
q4 --->|yes| a2
q3 ---->|no| a2(["**Non-cohesive**"])
q5 -->|yes| a1
q5 -->|no| a2
```
### Dry coherence {#sec-cn-dryco}
*Procedure*
1. Remould a 30 mm test sample into a cube, and air-dry.
2. If the cube collapses under its own weight or after being lightly touched, treat the soil as non-cohesive.
## Strength {#sec-cn-str}
Strength is also known as 'resistance to crushing'. This is assessed using hand or body-weight strength, so the user must calibrate themselves against the classes in @tbl-cn-str. @drohan2020 discuss various options for calibration, including the use of pinch gauges or push-pull gauges to learn what different levels of force feel like.
Each of the tests in this section are evaluated against @tbl-cn-str.
```{r}
#| label: tbl-cn-str
#| tbl-cap: "Strength (resistance to crushing) classes"
dat_cn_str <-
tribble(~Code, ~Name, ~Failure_cond, ~amt_force_n,
1, 'Very Weak', 'Very gentle force in hand', '< 8',
2, 'Weak', 'Gentle force in hand', '8-20',
3, 'Slightly firm', 'Moderate force in hand', '20-40',
4, 'Firm', 'Strong/maximum force in hand', '40-75',
5, 'Very firm', 'Gentle force underfoot', '75-150',
6, 'Hard', 'Full body weight (~80 kg) applied slowly', '150-800',
7, 'Very hard', 'Withstands full body weight', '> 800'
)
tbl_cn_str <- gt(dat_cn_str) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_label(Failure_cond = 'Failure condition',
amt_force_n = 'Force required (N)') |>
cols_width(Code ~pct(10), Name ~pct(20), amt_force_n ~pct(20))
tbl_cn_str
```
### Unconfined soil strength {#sec-cn-stru}
- Test at observed field moisture condition.
- If a test cube cannot be formed, the result is [1]{.ceg} 'Very Weak' (see @tbl-cn-str). This can happen when soil pedality is weak or absent, but also when pedality is strong and peds are small.
- This test cannot be reliably performed on auger-extracted samples.
*Procedure*
1. Perform the test on a minimally disturbed 30 mm cube.
2. Hold the cube between the thumb and forefinger. Both digits must be straight and fully extended.
3. Pinch down. If the cube can be crushed, rate the difficulty using categories [1-4]{.ceg} in @tbl-cn-str.
4. If the cube cannot be crushed by hand, attempt to crush it slowly underfoot, against a hard surface. Rate the difficulty using categories [5-7]{.ceg} in @tbl-cn-str.
### Unconfined aggregate strength {#sec-cn-stra}
- Test at observed field moisture condition.
- Test on whole peds where they are under 50 mm in size. Larger peds should be shaved down to 30 mm.
- This test cannot be reliably performed on auger-extracted samples.
*Procedure*
1. Perform the test on an extracted ped.
2. Hold the ped between the thumb and forefinger. Both digits must be straight and fully extended.
3. Pinch down. If the ped can be crushed, rate the difficulty using categories [1-4]{.ceg} in @tbl-cn-str.
4. If the ped cannot be crushed by hand, attempt to crush it slowly underfoot, against a hard surface. Rate the difficulty using categories [5-7]{.ceg} in @tbl-cn-str.
### Remoulded strength {#sec-cn-strr}
Some soils lose strength to a notable degree when remoulded, and their apparent clay content as estimated with hand texturing increases. This has implications for engineering.
- Test at observed field moisture condition.
- Perform the test on an extracted 30 mm cube or sample of equivalent volume.
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Perform the test on an extracted 30 mm cube or sample of equivalent volume.
2. Place the sample in a small plastic bag and seal with the air excluded (this maintains field moisture content while remoulding). Work the sample until its structure is completely broken down. This may take several minutes.
3. Still in the bag, remould the soil into a cube and assess its strength against @tbl-cn-str.
4. Use @tbl-cn-sens to also record the ratio of unconfined to remoulded strength ('sensitivity', @sec-cn-sens).
### Strength at plastic limit {#sec-cn-strp}
Soil strength at the plastic limit has engineering implications.
- Test at the soil's plastic limit.
- Perform the test on an extracted 30 mm cube or sample of equivalent volume.
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Work the sample until its structure is completely broken down. This may take several minutes. Keep adding small amounts of water so that the sample is almost, but not quite, saturated.
2. Remould the soil into a cube and assess its strength against @tbl-cn-str.
## Sensitivity {#sec-cn-sens}
In soils with an unconfined strength class of [4]{.ceg} firm or greater, sensitivity is reported as the ratio of unconfined soil strength (@sec-cn-stru) to remoulded strength (@sec-cn-strr). For weaker soils, the 'shear test' is performed. The two methods are assigned equivalent classes in @tbl-cn-sens.
- Test soil at a moist or wet state.
- Perform the test on a minimally disturbed 30 mm sample cube.
- This test cannot be reliably performed on auger-extracted samples.
*Procedure*
1. Hold the sample cube between extended thumb and forefinger as for @sec-cn-str.
2. Pinch and press the sample to create a lateral, 'shear' force, moving the finger forward and down over the thumb.
3. Assess the sample behaviour against @tbl-cn-sens.
Note that this test is not analogous to the shear vane test of @newzealandgeotechnicalsociety2005 and cannot be used as a substitute.
```{r}
#| label: tbl-cn-sens
#| tbl-cap: "Sensitivity (strength loss on remoulding) classes"
dat_cn_sens <-
tribble(~Code, ~Name, ~rel_loss, ~Description,
1, 'Non-sensitive', '0-1', 'the sample does not smear under shear force, and may soften only slightly',
2, 'Weakly sensitive', '2', 'the sample smears and skids under moderate shear force (20-40 kPa)',
3, 'Moderately sensitive', '3', 'the sample suddenly turns fluid under moderate shear force (20-40 kPa) and the fingers skid. Some free water is evident on fingers after shearing',
4, 'Very sensitive', '>3', 'the soil suddenly turns fluid and slippery under only gentle shear force (<20 kPa). Free water is easily seen on the fingers after shearing')
tbl_cn_sens <- gt(dat_cn_sens) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_label(rel_loss = 'Relative strength loss on remoulding (classes)',
Description = 'Shear test behaviour') |>
cols_width(Code ~pct(10), Name ~pct(20), rel_loss ~pct(20))
tbl_cn_sens
```
## Plasticity {#sec-cn-pla}
[Plasticity is the capacity of soil material to change shape continuously when stress is applied and to retain that shape after the removal of stress.]{.milne}
- Test soil at a wet state.
- Perform the test on 3-4 cm^2^ of soil.
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Thoroughly remould the sample, keeping it in a wet state.
2. Adjust the water content to slightly above the plastic limit. [In practice this water content is slightly above that at which a 4-mm diameter roll of sample crumbles but less than that when sample becomes sticky (@sec-cn-sti), if stickiness is exhibited.]{.milne}
3. Attempt to roll the sample out into a rod of 40 mm length. Assess the minimum achievable diameter of the rod and its behaviour using @tbl-cn-plas.
```{r}
#| label: tbl-cn-plas
#| tbl-cap: "Plasticity classes"
dat_cn_plas <-
tribble(~Code, ~Name, ~Description,
1, 'Non-plastic', 'A roll 40 mm long and 6 mm thick that supports its own weight cannot be formed.',
2, 'Slightly plastic', 'A roll 40 mm long and 6 mm thick can be formed and will support its own weight, but a roll 4 mm thick will not support its own weight.',
3, 'Moderately plastic', 'A roll 40 mm long and 4 mm diameter can be formed, and will support its own weight, but a roll 2 mm thick will not support its own weight.',
4, 'Very plastic', 'A roll 40 mm long and 2 mm thick can be formed and will support its own weight.')
tbl_cn_plas <- gt(dat_cn_plas) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_plas
```
## Stickiness {#sec-cn-sti}
[Stickiness is the degree to which remoulded soil adheres to foreign objects.]{.milne}
- Test soil at a wet state.
- Perform the test on 3-4 cm^2^ of soil.
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Thoroughly remould the sample, keeping it in a wet state.
2. [Press the remoulded material between thumb and forefinger, and note its adherence to the fingers.]{.milne}
3. [Adjust the water content by working the sample in the hand to remove water, or by adding water as necessary to achieve the maximum stickiness that the material will exhibit]{.milne}
4. Assess maximum stickiness and record using @tbl-cn-stik.
```{r}
#| label: tbl-cn-stik
#| tbl-cap: "Stickiness classes"
dat_cn_stik <-
tribble(~Code, ~Name, ~Description,
1, 'Non-sticky', 'After release of pressure, practically no soil material adheres to the thumb or forefinger',
2, 'Slightly sticky', 'After release of pressure, soil material adheres perceptibly to both thumb and forefinger but, as the digits are separated, it tends to come off one or the other cleanly. The material is not stretched appreciably when the thumb and finger are separated',
3, 'Moderately sticky', 'After release of pressure, soil material adheres to both thumb and forefinger and tends to stretch somewhat and pull apart rather than pulling free from either digit',
4, 'Very sticky', 'After release of pressure, soil material adheres so strongly to both thumb and forefinger that it is decidedly stretched when they are separated, and finally pulls apart leaving part of the soil on thumb and part on the forefinger.')
tbl_cn_stik <- gt(dat_cn_stik) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_stik
```
## Dilatency
[Dilatancy occurs due to volume change during shearing and is used as a criterion for the distinguishing non-cohesive from cohesive soil materials.]{.milne}
- Test soil at a moist to wet state.
- Perform the test on 3-4 cm^2^ of soil.
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Adjust the soil to a moist to wet state.
2. Roll into a ball \~30 mm diameter.
3. Hold sample in upturned palm and slap the back of the hand containing the sample several times with the other hand.
[A dilatant reaction is shown by a shiny surface caused by water extrusion, and by a dull surface when the palm of the hand is folded to partly remould the sample, causing water to be drawn into the sample.]{.milne} Record dilatent behaviour as a binary, [true/false]{.ceg}.
## Penetration resistance
Penetration resistance is the capacity of the soil, in its natural confined state, to resist penetration by rigid objects. This property is commonly related to strength by empirical means (@tbl-cn-penr).
- This test requires a large pit or exposure
*Procedure*
1. Expose a soil profile.
2. Assess ease of penetrating a vertical face using @tbl-cn-penr.
```{r}
#| label: tbl-cn-penr
#| tbl-cap: "Penetration resistance classes"
dat_cn_penr <-
tribble(~Code, ~Name, ~Description, ~kpa,
1, 'Extremely low', 'Easily penetrated by fist', '0-500',
2, 'Very low', 'Easily penetrated by thumb', '500 - 1000',
3, 'Low', 'Readily indented by thumb but penetrated with considerable effort. Imprinted by finger with some effort.', '1000 - 1500',
4, 'Moderate', 'Readily indented by thumbnail', '1500-2200',
5, 'High', 'Barely imprinted by thumb or forefinger', '2200 - 3000',
6, 'Very high', 'Indented by thumbnail. No imprint by thumb or finger', '3100 - 4000',
7, 'Extremely high', 'Barely indented by thumbnail', '> 4000')
tbl_cn_penr <- gt(dat_cn_penr) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20), kpa ~pct(20))
tbl_cn_penr
```
## Particle Packing
Particle packing assesses the stability of a gravelly soil.
- Test only on gravelly soils where strength cannot be assessed
- This test requires a large pit or exposure
- Do not test at wet or saturated field moisture conditions, as this is unsafe
*Procedure*
1. Expose a gravelly soil profile.
2. Assess ease of excavating and maintaining a vertical face using @tbl-cn-pack.
```{r}
#| label: tbl-cn-pack
#| tbl-cap: "Particle-packing classes for gravelly soils"
dat_cn_fail <-
tribble(~Code, ~Name, ~Description,
1, 'Loose', 'Easily dislodged by spade or pick; does not maintain a vertical face',
2, 'Compact', 'Intermediate between loose and dense',
3, 'Dense', 'Difficult to dislodge except with spade and by removing individual fragments; maintains a stable vertical face',
4, 'Very dense', 'Very difficult to dislodge except by pick and removing individual fragments; maintains a stable vertical face')
tbl_cn_fail <- gt(dat_cn_fail) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_fail
```
## Mode of failure {#sec-cn-fail}
[Failure is the manner in which unconfined soil yields to increasing stress.]{.milne}
- Test at observed field moisture condition.
- Perform the test on a minimally disturbed 30 mm cube or aggregate.
- If diagnosing Oxidic or Cutanoxidic soil material for the NZSC, repeat the test under dry to wet moisture conditions.
*Procedure*
1. Perform the unconfined strength test according to @sec-cn-stru.
2. At strengths of 4 or less, mode of failure can be observed. Assess and record per @tbl-cn-fail.
```{r}
#| label: tbl-cn-fail
#| tbl-cap: "Failure mode classes"
dat_cn_fail <-
tribble(~Code, ~Name, ~Description,
'N', 'Not determinable', 'Soil is either too dry or too wet to reliably test',
'V', 'Very friable', 'Test specimen cannot be formed, or crumbles under very slight stress on crushing within the hand, into aggregates predominantly <2 mm in size. In most instances the test specimen is difficult to obtain.',
'F', 'Friable', 'Test sample cannot be formed, or crumbles under very slight stress on crushing within the hand, into aggregates predominantly >2 mm in size, or crumbles under slight stress on crushing within the hand into aggregates predominantly <2 mm in size.',
'B', 'Brittle', 'Under slowly increasing pressure between the extended thumb and forefinger, a test specimen retains its size and shape with few or no cracks until it fractures abruptly into aggregates predominantly > 2 mm in size.',
'S', 'Semi-deformable', 'Under increasing pressure between the extended thumb and forefinger the test specimen as a whole is perceptibly compressed in the direction along which pressure is exerted, but cracks develop and the specimen ruptures before it has been compressed to half its original thickness. Before rupture, parts crumble and fall away if the specimen is shaken while held between the thumb and forefinger.',
'D', 'Deformable', 'Under slowly increasing pressure between the extended thumb and forefinger, the test specimen can be compressed to at least half its original thickness without the appearance of cracks and without rupture.')
tbl_cn_fail <- gt(dat_cn_fail) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_fail
```
## Fluidity {#sec-cn-flu}
Fluidity tests whether saturated soils have an unconfined strength that is largely eliminated by saturation. Such materials were generally emplaced under water, have never been drained, have a fine texture that minimises gravity-based settling, and are not overlain by enough other sediment to have been compressed.
- Test soil at a saturated state.
- Only test soils that are saturated under field conditions.
- Perform the test on \~50 cm^2^ of soil (a large handful).
- This test can be reliably performed on auger-extracted samples.
*Procedure*
1. Extract the sample and squeeze firmly in the hand.
2. Evaluate the sample behaviour using @tbl-cn-fluid.
```{r}
#| label: tbl-cn-fluid
#| tbl-cap: "Fluidity classes"
dat_cn_fluid <-
tribble(~Code, ~Name, ~Description,
1, 'Slightly fluid', 'Some material tends to flow into the spaces between the fingers, but after full pressure is exerted most of the residue is left in the hand',
2, 'Moderately fluid', 'Soil material flows easily between the fingers, but a small residue is left in the hand after full pressure is exerted',
3, 'Very fluid', 'Soil material flows like a slightly viscous liquid between the fingers, and very little or no residue is left in the hand after full pressure is exerted')
tbl_cn_fluid <- gt(dat_cn_fluid) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_fluid
```
## Induration {#sec-cn-ind}
[Induration is the degree to which soil particles are held together by some combination of cementation and close packing.]{.milne}
- Perform the test on a minimally disturbed 30 mm cube or aggregate.
- This test may also be performed on individual nodules and other solids \< 30 mm.
- This test cannot be reliably performed on auger-extracted samples.
- This test requires a minimum one hour to complete so may be done immediately following fieldwork.
*Equipment*
- Sponge (\~50 mm diameter, flat)
- Deionised (DI) water
*Procedure*
1. Test the soil strength at field-moist condition according to @sec-cn-stru.
2. Place the sample cube on a wet sponge until thoroughly moistened, then immerse the sample in DI water for 1 hour.
3. Retest the soil strength of the wet sample according to @sec-cn-stru.
4. Assess the behaviour of the sample using @tbl-cn-ind.
```{r}
#| label: tbl-cn-ind
#| tbl-cap: "Induration classes"
dat_cn_ind <-
tribble(~Code, ~Name, ~Description,
1, 'Non-indurated', 'A wet test specimen slakes within one hour when placed in water',
2, 'Very weakly indurated', 'A wet test specimen that has been immersed for one hour and has not slaked has strength class of 2-4',
3, 'Weakly indurated', 'A wet test specimen that has been immersed for one hour has a strength class of 6',
4, 'Strongly indurated', 'A wet test specimen that has been immersed for an hour has a strength class of 7',
5, 'Very strongly indurated', 'A wet test specimen after immersion for an hour has a strength class of >7 and does not break when struck by a sharp blow with a hammer.')
tbl_cn_ind <- gt(dat_cn_ind) |>
tab_options(
column_labels.font.weight = 'bold',
heading.title.font.weight = 'bold',
table.align = 'center',
table.width = '85%'
) |>
tab_style(style = list(cell_text(color = 'red',
weight = 'bold',
align = 'center')),
locations = cells_body(columns = 1)) |>
cols_width(Code ~pct(10), Name ~pct(20))
tbl_cn_ind
```