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新唐書卷二十八上 志第十八上 曆四上

Volume 28A Treatises 18A: Calendar 4A

Chapter 28 of 新唐書 · New Book of Tang
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1
In computing the evolving era of the Kaiyuan Dayan calendar, the high origin falls in the year Yān-féng Kùn-dūn; reckoned back from Kaiyuan 12 (jiazi), the accumulated count is 96,961,740.
2
I. Method for Determining Central Qi and New Moons
3
Universal divisor: 3,040.
4
Year-fraction constant: 1,110,343.
5
New-moon constant: 89,773.
6
Reduction constant: 91,200.
7
Stalk remainder: 15,943.
8
Applied difference: 17,124.
9
Intercalation threshold: 87,018.
10
Three-origin interval: 15 stalks, remainder 664, 7 parts.
11
Four-image interval: 29 stalks, remainder 1,613.
12
Central-qi surplus fraction: 1,328, 14 parts.
13
New-moon void fraction: 1,427.
14
Hexagram line count: 60.
15
Image cycle: 24.
16
滿
Multiply the era count by the year-fraction constant to obtain the central accumulated parts. Divide by the universal divisor; the quotient is accumulated days. Remove full cycles of sixty lines; from the remainder, counting outward from jiazi, obtain the celestial central qi. The fractional parts become the minor remainder; the days become the major remainder. Add the three-origin interval to obtain the next qi. Whenever linked rates are added and fractional remainders remain below, combine them by kind. When a divisor is filled, carry upward step by step and add to the higher place. Cast out full cycles of sixty when days overflow.
17
滿 退
Divide the central accumulated parts by the new-moon constant; the remainder is the intercalation pendulum. Subtract that amount from the central accumulated parts to obtain the new-moon accumulated parts. Convert by the universal divisor into days; fix the era as before to obtain the canonical winter new moon. Add one four-image interval—seven days, remainder 1,163 lesser—to obtain the first quarter. Double it to obtain full moon. Triple it to obtain last quarter. Quadruple it—one full sorting—to obtain the next month’s new moon. In quartering remainders, one part is “lesser,” three are “greater.” Combine the central surplus and new-moon void fractions, steadily increasing the intercalation pendulum; each month the intercalation fraction diminishes. Whenever the intercalation pendulum reaches 56,760 or more, the year receives an intercalary month. Track the intercalation wane; when it exceeds the intercalation threshold, assign an intercalary month. Whether advancing or retreating, the rule is the fixed new moon in a month without central qi.
18
滿 滿
Whenever a regular qi’s minor remainder is less than the universal divisor and no more than half the central surplus fraction, multiply by the image cycle, include seconds, combine and quintuple, and subtract from the stalk substance; The remainder, divided by the stalk remainder, gives the days. Count outward from the first day of the regular qi; the result is the extinction day. Whenever a canonical new moon’s minor remainder is less than the new-moon void fraction, subtract the minor remainder from the universal divisor; double and quintuple the remainder; The remainder, divided by the new-moon void fraction, gives the days. Count outward from the first day of the canonical new moon; the result is the lunar extinguishing day.
19
II. Method for Issuing and Gathering In
20
Heaven-central interval: five stalks, remainder 221, 31 parts; Second divisor: 72.
21
Earth-central interval: six stalks, remainder 265, 86 parts; Second divisor: 120.
22
Zhen-hui interval: three stalks, remainder 132, 103 parts.
23
Chronogram divisor: 760.
24
Clepsydra divisor: 304.
25
For each, start from the mid-node of the central qi; obtain the first phenological hou. Add the heaven-central interval to obtain the next hou. Add again to obtain the last hou. Fix from the central qi; obtain when the duke hexagram governs. Keep adding the earth-central interval for successive hexagrams; or add the zhen-hui interval to the marquis hexagram to obtain when the outer hexagram of the twelve nodes governs. Fix from the four establishment days; obtain when spring Wood, summer Fire, autumn Metal, and winter Water govern. Subtract the zhen-hui interval from the last seasonal month’s central qi; obtain when Earth the King governs. Whenever addition or subtraction leaves unequal fractional denominators, cross-multiply numerators by the opposite denominators, then add or subtract; The product of denominators is the common divisor.
26
Regular qi · Month · Mid-node · Four cardinal hexagrams
27
First hou
28
Second hou
29
Last hou
30
Opening hexagram
31
Middle hexagram
32
Closing hexagram
33
Winter Solstice · eleventh month, mid-month · Kan ☵, first line
34
Earthworms coil up
35
Elk shed their antlers
36
Springs begin to stir
37
Duke · Zhōng Fú
38
Sovereign · Fù
39
Marquis · Zhūn (inner)
40
Lesser Cold · twelfth month, node · Kan ☵, second line
41
Wild geese fly north
42
Magpies begin to nest
43
Pheasants begin to call
44
Marquis · Zhūn (outer)
45
Great officer · Qiān
46
Minister · Kuí
47
Greater Cold · twelfth month, mid-month · Kan ☵, third line
48
Hens begin to brood
49
Birds of prey grow fierce
50
Ice hardens at the depths of the waters
51
Duke · Shēng
52
Sovereign · Lín
53
Marquis · Xiǎo Guò (inner)
54
Start of Spring · first month, node · Kan ☵, fourth line
55
The east wind melts the ice
56
Creatures in hibernation begin to stir
57
Fish appear beneath the ice
58
Marquis · Xiǎo Guò (outer)
59
Great officer · Méng
60
Minister · Yì
61
Rain Water · first month, mid-month · Kan ☵, fifth line
62
Otters present fish
63
Wild geese return
64
Plants put forth buds
65
Duke · Jiàn
66
Sovereign · Tài
67
Marquis · Xū (inner)
68
Awakening of Insects · second month, node · Kan ☵, sixth line
69
Peaches begin to blossom
70
Orioles begin to sing
71
Hawks transform into turtledoves
72
Marquis · Xū, outer
73
Great officer · Suí
74
Minister · Jìn
75
Spring Equinox · second month, mid-month · Zhèn ☳, first line
76
Swallows return
77
Thunder begins to sound
78
Lightning first appears
79
Duke · Xiè
80
Sovereign · Dà Zhuàng
81
Marquis · Yù, inner
82
Pure Brightness · third month, node · Zhèn ☳, second line
83
Paulownia begins to flower
84
Field mice transform into quails
85
Rainbows first appear
86
Marquis · Yù, outer
87
Great officer · Sòng
88
Minister · Gǔ
89
Grain Rain · third month, mid-month · Zhèn ☳, third line
90
Duckweed begins to grow
91
Cuckoos smooth their feathers
92
Hoopoes descend upon the mulberries
93
Duke · Gé
94
Sovereign · Shǐ
95
Marquis · Lǚ, inner
96
Start of Summer · fourth month, node · Zhèn ☳, fourth line
97
Mole-crickets begin to chirp
98
Earthworms come forth
99
Snake-gourds begin to grow
100
Marquis · Lǚ, outer
101
Great officer · Shī
102
Minister · Bǐ
103
滿
Lesser Fullness · fourth month, mid-month · Zhèn ☳, fifth line
104
Bitter greens come into flower
105
Tender grasses wither
106
Lesser heat arrives
107
Duke · Xiǎo Xù
108
Sovereign · Qián
109
Marquis · Dà Yǒu, inner
110
Grain in Ear · fifth month, node · Zhèn ☳, sixth line
111
Praying mantises hatch
112
Shrikes begin to call
113
The mockingbirds fall silent
114
Marquis · Dà Yǒu, outer
115
Great officer · Jiā Rén
116
Minister · Jǐng
117
Summer Solstice · fifth month, mid-month · Lí ☲, first line
118
鹿
Deer shed their antlers
119
Cicadas begin to chirp
120
Pinellia comes into growth
121
Duke · Xián
122
Sovereign · Gòu
123
Marquis · Dǐng, inner
124
Lesser Heat · sixth month, node · Lí ☲, second line
125
Warm winds arrive
126
Crickets take to the walls
127
Hawks begin to learn flight
128
Marquis · Dǐng, outer
129
Great officer · Fēng
130
Minister · Huàn
131
Greater Heat · sixth month, mid-month · Lí ☲, third line
132
Rotting grass turns into fireflies
133
The earth is damp with sultry heat
134
Heavy rains fall at intervals
135
Duke · Lǚ
136
Sovereign · Dùn
137
Marquis · Héng, inner
138
Start of Autumn · seventh month, node · Lí ☲, fourth line
139
Cool winds arrive
140
White dew falls
141
Cold cicadas begin to chirp
142
Marquis · Héng, outer
143
Great officer · Jié
144
Minister · Tóng Rén
145
End of Heat · seventh month, mid-month · Lí ☲, fifth line
146
Hawks present their catch
147
Heaven and earth begin to turn austere
148
The grain ripens
149
Duke · Sǔn
150
Sovereign · Pǐ
151
Marquis · Xùn, inner
152
White Dew · eighth month, node · Lí ☲, sixth line
153
Wild geese return
154
Swallows depart
155
Birds gather stores of food
156
Marquis · Xùn, outer
157
Great officer · Cuì
158
Minister · Dà Chù
159
Autumn Equinox · eighth month, mid-month · Duì ☱, first line
160
Thunder falls silent
161
Creatures in hibernation close their burrows
162
The waters begin to recede
163
Duke · Bì
164
Sovereign · Guān
165
Marquis · Guī Mèi, inner
166
Cold Dew · ninth month, node · Duì ☱, second line
167
The guest geese arrive
168
Sparrows dive into the waters and become clams
169
Chrysanthemums show yellow blossoms
170
Marquis · Guī Mèi, outer
171
Great officer · Wú Wàng
172
Minister · Míng Yí
173
Frost Descent · ninth month, mid-month · Duì ☱, third line
174
Wolves present their kill
175
Grasses and trees turn yellow and shed their leaves
176
Creatures in hibernation all lie low
177
Duke · Kùn
178
Sovereign · Bō
179
Marquis · Gèn, inner
180
Start of Winter · tenth month, node · Duì ☱, fourth line
181
The waters begin to freeze
182
The ground begins to harden with frost
183
Pheasants enter the waters and become great clams
184
Marquis · Gèn, outer
185
Great officer · Jì Jì
186
Minister · Shì Kè
187
Lesser Snow · tenth month, mid-month · Duì ☱, fifth line
188
Rainbows are no longer seen
189
The qi of heaven ascends and the qi of earth descends
190
All is shut in, and winter takes hold
191
Duke · Dà Guò
192
Sovereign · Kūn
193
Marquis · Wèi Jì, inner
194
Greater Snow · eleventh month, node · Duì ☱, sixth line
195
Otters fall silent
196
Tigers begin to mate
197
Litchi sprouts break forth
198
Marquis · Wèi Jì, outer
199
Great officer · Jiǎn
200
Minister · Yí
201
滿 滿
For each month, divide the intercalation wane by the universal divisor to obtain days, yielding the interval from central qi to canonical new moon. To determine hexagrams and phenological hou, cumulatively add or subtract the heaven- and earth-central intervals. When fixing the time of issuing and gathering in, set each minor remainder, multiply by six lines, and divide by the chronogram divisor to obtain the half-chronogram count. The remainder, divided by three, gives fractional parts. When the parts fill the clepsydra divisor, they become clepsydra notches. If the image accumulation is to fill clepsydra marks directly, take the remainder, multiply by ten, and divide by nineteen for the parts. Fix the chronogram from the half-period of zi, counting outward from the tally.
202
III. Method for Determining Solar Motion
203
Circuit-of-heaven constant: 1,110,379 and greater.
204
Degrees in the circuit of heaven: 365, void fraction 779 and greater.
205
Precession per year: 36 and greater.
206
Fixed qi
207
Expansion and contraction fractions
208
Lead and lag counts
209
Rates of increase and decrease
210
Lunar elongation accumulation
211
Winter Solstice
212
Expansion: 2,353
213
Leading edge
214
Increase rate: 176
215
Waning phase, initial
216
Lesser Cold
217
Expansion: 1,845
218
Lead count: 2,353
219
Increase rate: 138
220
Waning accumulation: 176
221
Greater Cold
222
Expansion: 1,390
223
Lead count: 4,198
224
Increase rate: 104
225
Waning accumulation: 314
226
Start of Spring
227
Expansion: 976
228
Lead count: 5,588
229
Increase rate: 73
230
Waning accumulation: 418
231
Rain Water
232
Expansion: 588
233
Lead count: 6,564
234
Increase rate: 44
235
Waning accumulation: 491
236
Awakening of Insects
237
Expansion: 214
238
Lead count: 7,152
239
Increase rate: 16
240
Waning accumulation: 535
241
Spring Equinox
242
Contraction: 214
243
Lead count: 7,366
244
Decrease rate: 16
245
Waning accumulation: 551
246
Pure Brightness
247
Contraction: 588
248
Lead count: 7,152
249
Decrease rate: 44
250
Waning accumulation: 535
251
Grain Rain
252
Contraction: 976
253
Lead count: 6,564
254
Decrease rate: 73
255
Waning accumulation: 491
256
Start of Summer
257
Contraction: 1,390
258
Lead count: 5,588
259
Decrease rate: 104
260
Waning accumulation: 418
261
滿
Lesser Fullness
262
Contraction: 1,845
263
Lead count: 4,198
264
Decrease rate: 138
265
Waning accumulation: 314
266
Grain in Ear
267
Contraction: 2,353
268
Lead count: 2,353
269
Decrease rate: 176
270
Waning accumulation: 176
271
Summer Solstice
272
Contraction: 2,353
273
Trailing edge
274
Increase rate: 176
275
Waxing phase, initial
276
Lesser Heat
277
Contraction: 1,845
278
Lag count: 2,353
279
Increase rate: 138
280
Waxing accumulation: 176
281
Greater Heat
282
Contraction: 1,390
283
Lag count: 4,198
284
Increase rate: 104
285
Waxing accumulation: 314
286
Start of Autumn
287
Contraction: 976
288
Lag count: 5,588
289
Increase rate: 73
290
Waxing accumulation: 418
291
End of Heat
292
Contraction: 588
293
Lag count: 6,564
294
Increase rate: 44
295
Waxing accumulation: 491
296
White Dew
297
Contraction: 214
298
Lag count: 7,152
299
Increase rate: 16
300
Waxing accumulation: 535
301
Autumn Equinox
302
Expansion: 214
303
Lag count: 7,366
304
Decrease rate: 16
305
Waxing accumulation: 551
306
Cold Dew
307
Expansion: 588
308
Lag count: 7,152
309
Decrease rate: 44
310
Waxing accumulation: 535
311
Frost Descent
312
Expansion: 976
313
Lag count: 6,564
314
Decrease rate: 73
315
Waxing accumulation: 491
316
Start of Winter
317
Expansion: 1,390
318
Lag count: 5,588
319
Decrease rate: 104
320
Waxing accumulation: 418
321
Lesser Snow
322
Expansion: 1,845
323
Lag count: 4,198
324
Decrease rate: 138
325
Waxing accumulation: 314
326
Greater Snow
327
Expansion: 2,353
328
Lag count: 2,353
329
Decrease rate: 176
330
Waxing accumulation: 176
331
滿退 滿退
Apply the expansion–contraction fractions: subtract where expansion and add where contraction from the three-origin tally, yielding the days and remainder for fixed qi. Multiply the days by twelve, triple the minor remainder, divide by the chronogram divisor and add the quotient, to obtain the fixed-qi chronogram count. The remainder, multiplied by ten and reduced again, gives fractional parts. Combine the expansion–contraction fractions of the current and next qi, double and multiply by six lines, divide by the sum of their chronogram counts, and obtain the terminal rate. Set out both qi’s expansion–contraction fractions, each doubled and multiplied by six lines, and divide each by its chronogram count. Subtract the smaller from the larger; the remainder is the qi difference. After a solstice, add the difference to the terminal rate; after an equinox, subtract it—this yields the initial rate. Double the qi difference, double and multiply by six lines, divide again by the combined chronogram counts of both qi, and obtain the day difference. Halve the day difference and add or subtract from the initial and terminal rates to obtain the fixed rates. Using the day difference, subtract from the initial fixed rate after a solstice and add after an equinox, yielding the daily expansion–contraction fraction. Accumulate stepwise: for each day within the entered qi, add or subtract the lead and lag counts listed under that qi to obtain each day’s fixed tally. To determine waxing and waning accumulations, follow the same procedure. After the Winter Solstice is yang recovery: add in expansion and subtract in contraction. After the Summer Solstice is yin recovery: add in contraction and subtract in expansion. For the qi immediately before each cardinal solstice or equinox, at the yin–yang transition the rates cannot be merged; use the prior qi’s terminal rate as the initial rate. Before a solstice add the difference to obtain the terminal rate; before an equinox subtract it. For the rest, follow the method above; each quantity sought is thereby obtained. When fractional parts do not make a full unit and each qi has a different denominator, reduce by retreating the divisor. Use one hundred as the denominator; at one-half or above, round up to one. At the Winter and Summer Solstices alike the sun reaches the cosmological mean; there is neither expansion nor contraction. For the remaining qi, first subtract then add the lead and lag counts under each qi to the regular qi’s minor remainder; carry or borrow days as needed to obtain fixed major and minor remainders. All calculations of solar and lunar longitude, orbital motion, clepsydra marks, and eclipses use fixed qi. Published calendars follow regular qi. Reduce the canonical new, quarter, and full moons by each entered day count. If the major remainder is too small to subtract, add sixty lines, then subtract. Subtract one from the entered fixed-qi day count, multiply by the day difference, and halve. If the prior fraction is smaller, add; if larger, subtract from the qi’s initial fixed rate; then multiply by the entered fixed-qi day count, remainder, and seconds. In every division, first unify whole units through the denominator, include the numerator, then multiply. Multiply and divide by the denominators. Use the result to adjust the waxing–waning accumulation, obtaining each entered waxing–waning fixed tally. When new or full moon is not an eclipse syzygy, multiply the entered day count by twelve. Triple the minor remainder, divide by the chronogram divisor, and add the quotient; Multiply by the rate of increase or decrease, and divide by the fixed-qi chronogram count. Use the result to adjust the anomalistic accumulation, yielding a fixed value for each entry.
332
觿輿 觿輿宿
Southern Dipper: 26°; Ox: 8°; Maid: 12°; Emptiness: 10°, void fraction 779 and greater. Rooftop 17°, Encampment 16°, Eastern Wall 9°, Stride 16°, Bond 12°, Stomach 14°, Hairy Head 11°, Net 17°, Turtle Beak 1°, Three Stars 10°, Eastern Well 33°, Ghost Cart 3°, Willow 15°, Seven Stars 7°, Extended Net 18°, Wings 18°, Chariot Shaft 17°, Horn 12°, Neck 9°, Root 15°, Room 5°, Heart 5°, Tail 18°, Winnowing Basket 11° — the equatorial lodge degrees. The arc-degrees assigned to Net, Turtle Beak, Three Stars, and Ghost Cart differ from the ancient reckoning. They were fixed by armillary measurement against the sky and adopted as standard constants. The celestial girdle runs through heaven’s center; the polar axis of the instrument is the reference for laying out the ecliptic.
333
滿
To find where the winter-solstice precession applies: take five degrees on either side of the solstice as one band; begin at twelve and subtract one for each successive band. After nine bands the tally reaches four. At the two Establishment qi, treat one degree as slightly strong and use the mean value. From before the spring equinox and after the autumn equinox, begin the first band at four and add one per band; after nine bands the tally is twelve, and the ecliptic obliquity cycle completes. For the interval after the spring equinox and before the autumn equinox, use the same five-degree bands. Begin at twelve; after nine bands the tally reaches four. At the two Establishment qi, treat one degree as slightly strong and use the mean value. Before and after the summer solstice, begin the first band at four; after nine bands the tally is twelve. Accumulate the trims in order, multiply the band index by the limit value, and divide by 120 to obtain degrees. The remainder, divided by twelve, gives fractional parts. If divided by ten instead, use twelve as the denominator for major parts, naming greater, half, lesser, strong, and weak fractions. This is called the ecliptic–equator difference. Within nine bands on either side of each solstice, subtract the difference from the equatorial longitude; within nine bands on either side of each equinox, add it — yielding ecliptic longitude in each case.
334
觿輿 宿 使
Kaiyuan year 12: Southern Dipper 23½°, Ox 7½°, Maid 11° lesser, Emptiness 10°, six Emptiness-difference parts 19 greater. Rooftop 17° greater, Encampment 17° lesser, Eastern Wall 9° greater, Stride 17½°, Bond 12° greater, Stomach 14° greater, Hairy Head 11°, Net 16° lesser, Turtle Beak 1°, Three Stars 9° lesser, Eastern Well 30°, Ghost Cart 2° greater, Willow 14° lesser, Seven Stars 6° greater, Extended Net 18° greater, Wings 19° lesser, Chariot Shaft 18° greater, Horn 13°, Neck 9½°, Root 15° greater, Room 5°, Heart 4° greater, Tail 17°, Winnowing Basket 10° lesser — the ecliptic lodge degrees used to pace the sun’s daily course. The moon and the five planets are reckoned by the same ecliptic framework. These lodge longitudes all carry fractional remainders; successive reckonings round them to lesser, half, or greater parts to align with whole degrees. To verify against past ages and test future ones, apply the precession: for each degree of shift, recalculate by the method to obtain contemporary longitudes — only then may one pace the sun, moon, and planets.
335
宿滿宿
Subtract the circuit-of-heaven constant from the central accumulation; The remainder, divided by the universal divisor, gives degrees. Count from equatorial Emptiness 9°, subtracting whole lodges and the Emptiness fraction in turn, until less than one lodge remains beyond the tally — this yields the solar longitude at winter-solstice hour-addition. Add the three-origin interval repeatedly to obtain the hour-added solar degree for each successive qi.
336
滿 滿 宿
Subtract the degree remainder from the universal divisor; Multiply the remainder by the band index for the winter-solstice solar station’s distance entry to obtain the pre-distance fraction. Take the ecliptic–equator difference for the distance band, multiply by the universal divisor, and subtract the pre-distance fraction; When the remainder fills 120, divide to obtain the fixed difference. If it does not fill, multiply by the image cycle and divide again to obtain seconds and parts. Subtract the fixed difference from the equatorial lodge longitude to obtain the ecliptic solar degree at winter-solstice hour-addition.
337
滿 宿
Set the annual precession, multiply by the band index, and divide by 120 for seconds and parts. The remainder becomes minor parts. Add this to the three-origin interval and accumulate the trims in order. Count through the ecliptic lodges in sequence to obtain the hour-added solar degree for each fixed qi.
338
滿
Set the fixed minor remainder for that qi and keep a duplicate tally. Multiply by its daily equation of time, divide by the universal divisor, and add or subtract from the duplicate according to surplus or deficit. Subtract this from the day’s hour-added degree remainder to obtain the solar longitude at midnight. Add one interval at each step; apply each day’s equation to the degree remainder by addition or subtraction — yielding the midnight solar degree day by day.
339
IV. Method for Determining Lunar Motion
340
Rotation cycle constant: 670,1279.
341
Rotation cycle: 27 days, remainder 1,685, 79 seconds.
342
Rotation divisor: 76.
343
Rotation second divisor: 80.
344
滿
Multiply the new-moon accumulation by the second divisor and cast out full rotation cycles; Reduce the remainder again by the second divisor to obtain rotation entry parts; When the parts fill the universal divisor, they become days. Count outward from the day tally to obtain the rotation entry at the hour-added canonical new moon of the celestial first month. Add the rotation increment of one day, remainder 2,967, and one second to obtain the next new moon. Add one four-image interval in turn to obtain the first and last quarters. When days and remainder-seconds fill the rotation cycle, cast them out. Subtract each new-moon, quarter, or full-moon minor remainder to obtain the rotation entry at that night’s midnight.
345
Rotation day
346
Rotation parts
347
Column decrement
348
Accumulated rotation degrees
349
Rates of increase and decrease
350
Anomalistic accumulation
351
Day 1
352
917
353
Tabular advance: 13
354
Rotation degrees, initial
355
Increase rate: 297
356
Waning accumulation, initial
357
Day 2
358
930
359
Tabular advance: 13
360
12° 5 parts
361
Increase rate: 259
362
Waning accumulation: 297
363
Day 3
364
943
365
Tabular advance: 13
366
24° 23 parts
367
Increase rate: 220
368
Waning accumulation: 556
369
Day 4
370
956
371
Tabular advance: 14
372
36° 54 parts
373
Increase rate: 180
374
Waning accumulation: 776
375
Day 5
376
970
377
Tabular advance: 14
378
49° 22 parts
379
Increase rate: 139
380
Waning accumulation: 956
381
Day 6
382
984
383
Tabular advance: 16
384
62° 4 parts
385
Increase rate: 97
386
Waning accumulation: 1,095
387
Day 7
388
1,000
389
Tabular advance: 18
390
75°, void
391
Initial increase rate: 48, terminal decrease rate: 6
392
Slow accumulation: 1,192
393
Day 8
394
1,018
395
Tabular advance: 19
396
88° 12 parts
397
Decrease rate: 64
398
Slow accumulation: 1,234
399
Day 9
400
1,037
401
Tabular advance: 14
402
101° 42 parts
403
Decrease rate: 106
404
Slow accumulation: 1,170
405
Day 10
406
1,051
407
Tabular advance: 14
408
115° 15 parts
409
Decrease rate: 148
410
Slow accumulation: 1,064
411
Day 11
412
1,065
413
Tabular advance: 14
414
129° 2 parts
415
Decrease rate: 189
416
Slow accumulation: 916
417
Day 12
418
1,079
419
Tabular advance: 13
420
143° 3 parts
421
Decrease rate: 229
422
Slow accumulation: 727
423
Day 13
424
1,092
425
Tabular advance: 13
426
157° 18 parts
427
Decrease rate: 267
428
Slow accumulation: 498
429
Day 14
430
1,105
431
退
Tabular advance: 10, retreat: 3
432
171° 46 parts
433
Initial decrease rate: 231, terminal increase rate: 66
434
Slow accumulation: 231
435
Day 15
436
1,112
437
退
Tabular retreat: 13
438
186° 11 parts
439
Increase rate: 289
440
Fast accumulation: 66
441
Day 16
442
1,099
443
退
Tabular retreat: 13
444
200° 59 parts
445
Increase rate: 250
446
Fast accumulation: 355
447
Day 17
448
1,086
449
退
Tabular retreat: 13
450
215° 18 parts
451
Increase rate: 211
452
Fast accumulation: 605
453
Day 18
454
1,073
455
退
Tabular retreat: 14
456
229° 40 parts
457
Increase rate: 171
458
Fast accumulation: 816
459
Day 19
460
1,059
461
退
Tabular retreat: 14
462
243° 49 parts
463
Increase rate: 130
464
Fast accumulation: 987
465
Day 20
466
1,045
467
退
Tabular retreat: 17
468
257° 44 parts
469
Increase rate: 87
470
Fast accumulation: 1,117
471
Day 21
472
1,028
473
退
Tabular retreat: 18
474
271° 25 parts
475
Initial increase rate: 36, terminal decrease rate: 18
476
Fast accumulation: 1,204
477
Day 22
478
1,010
479
退
Tabular retreat: 18
480
284° 65 parts
481
Decrease rate: 73
482
Fast accumulation: 1,222
483
Day 23
484
992
485
退
Tabular retreat: 14
486
298° 11 parts
487
Decrease rate: 116
488
Fast accumulation: 1,149
489
Day 24
490
978
491
退
Tabular retreat: 14
492
311° 15 parts
493
Decrease rate: 157
494
Fast accumulation: 1,033
495
Day 25
496
964
497
退
Tabular retreat: 14
498
324° 5 parts
499
Decrease rate: 198
500
Fast accumulation: 876
501
Day 26
502
950
503
退
Tabular retreat: 13
504
336° 57 parts
505
Decrease rate: 237
506
Fast accumulation: 678
507
Day 27
508
937
509
退
Tabular retreat: 13
510
349° 19 parts
511
Decrease rate: 276
512
Fast accumulation: 441
513
Day 28
514
924
515
退
Tabular retreat: 7, advance: 6
516
361° 44 parts
517
Initial decrease rate: 165, terminal increase rate enters thereafter
518
Fast accumulation: 165
519
退
For each syzygy, set the increase-decrease rates for the entered rotation days at new, quarter, and full moon; average them with the following rate to obtain the universal rate. Subtract the two rates; the remainder is the rate difference. If the prior rate is larger, subtract the entry remainder from the universal divisor, multiply the remainder by the rate difference, divide by the universal divisor and round up, then halve together with the rate difference; If the prior rate is smaller, halve the entry remainder, multiply by the rate difference, and divide by the universal divisor likewise: this yields the hour-added rotation rate. Halve this and apply increase or decrease to the hour entry; the remainder is the rotation remainder. For the rotation remainder, when increase applies, subtract from the divisor; when decrease applies, use the remainder as basis: multiply by the rate difference, divide by the universal divisor and add to the universal rate; multiply by the rotation rate and reduce by the universal divisor; subtract for fast and add for slow to the rotation rate, obtaining the fixed rate. Apply the fixed rate to adjust the anomalistic accumulation, yielding the fixed number. When no matching rate follows, proceed from the prior rate in the same way. When increase applies, take the universal rate as the initial value and subtract half the rate difference; when decrease applies, the universal rate itself serves. When adjustment of the entry remainder carries or borrows a day, apportion the parts over two days and compute by initial or terminal remainder as the method requires. Use the result together to adjust the rotation rate. This procedure derives from the Huangji calendar, refining the subtle variations of computational astronomy. When new or full moon has no eclipse, multiply the entry remainder directly by the increase-decrease rate, divide by the universal divisor, and adjust fast-slow accordingly to obtain the fixed number.
520
Day 7: initial value 2,701, terminal value 339. Day 14: initial value 2,363, terminal value 677. Day 21: initial value 2,024, terminal value 1,016. Day 28: initial value 1,686, terminal value 1,354. Divide the rotation cycle by the four-image divisor; each segment is six days, 2,701 parts. Reduce the full count to approximate eight parts in nine of a day. For each segment, subtract from the divisor; the remainder is the terminal value. Accumulate the four-image transitions in order, yielding each corresponding day’s initial and terminal values. If the entered rotation remainder falls below the initial value, apply increase or decrease following the prior rate. If above the initial value, reverse the decline and revert to the posterior rate.
521
退 退使
Set the major and minor remainders for each new, quarter, and full moon; apply the fixed fast-slow numbers for entered qi and rotation—subtract for fast, add for slow—to obtain the fixed syzygy remainders. When the fixed new-moon day name matches the next new moon, the month is long; when they differ, it is short; when no central qi falls in the month, it is intercalary. All references to midnight begin from true midnight at the start of zi before dawn. In calendar annotation, if the fixed minor remainder at quarter or full moon does not reach the early-morning initial remainder, set the date back one day. The same applies when a full-moon eclipse begins before early morning. Because the moon’s nine-path motion varies in speed, months naturally run three long and two short. Cumulative adjustment by the sun’s daily equation of time can occasionally yield four long and three short months; the arithmetic permits it. In practice, inspect whether the hour-added time is early or late and adjust accordingly, keeping within three long and three short months. When the first-month new moon has an eclipse at exact visibility, adjust long-short assignment a month or two on either side so that waning falls on the last or second day. For each fixed syzygy at midnight, name the solar longitude from that day’s degree and remainder. Array the fixed new- and full-moon minor remainders and keep duplicate tallies. Multiply by that day’s equation of time, divide by the universal divisor, and add or subtract from the duplicate according to surplus or deficit. Add to the midnight solar longitude to obtain the hour-added solar degree for each.
522
宿 宿 宿 宿西 宿西 宿 宿 宿西 宿 宿 宿 宿 滿 宿
At syzygy, when winter falls in yin months and summer in yang months, the moon follows the green path; After the Winter and Summer Solstices, the green path’s half-intersection lies at the spring-equinox lodge, east of the ecliptic. After Start of Winter and Start of Summer, the green path’s half-intersection lies at the Start-of-Spring lodge, southeast of the ecliptic. At the opposing lodge, the same applies. When winter is in yang months and summer in yin months, the moon follows the white path; After the Winter and Summer Solstices, the white path’s half-intersection lies at the autumn-equinox lodge, west of the ecliptic. After Start of Winter and Start of Summer, the white path’s half-intersection lies at the Start-of-Autumn lodge, northwest of the ecliptic. At the opposing lodge, the same applies. When spring is in yang months and autumn in yin months, the moon follows the vermilion path; After the Spring and Autumn Equinoxes, the vermilion path’s half-intersection lies at the summer-solstice lodge, south of the ecliptic. After Start of Spring and Start of Autumn, the vermilion path’s half-intersection lies at the Start-of-Summer lodge, southwest of the ecliptic. At the opposing lodge, the same applies. When spring is in yin months and autumn in yang months, the moon follows the black path. After the Spring and Autumn Equinoxes, the black path’s half-intersection lies at the winter-solstice lodge, north of the ecliptic. After Start of Spring and Start of Autumn, the black path’s half-intersection lies at the Start-of-Winter lodge, northeast of the ecliptic. At the opposing lodge, the same applies. The four seasons yield eight nodes; at each yin–yang crossing the moon meets the ecliptic — hence nine paths of lunar motion. For each conjunction entry, take the ecliptic solar degree at the initial and middle of the seventy-two hou; every five degrees is one band, beginning at twelve and subtracting one per band until four, then one degree slightly strong—use the mean. Begin again at four; add one per band until twelve at half-intersection, six degrees from the ecliptic. From twelve again, subtract one per band until four, likewise one degree slightly strong—use the mean. Begin at four again; add one per band until twelve, reuniting with the solar track. Accumulate the counts in order, multiply by the band index, and divide by 240 to obtain degrees. The remainder, divided by twenty-four, gives parts; if divided by twenty instead, major parts use twelve as denominator. This is the lunar ecliptic latitude difference. Within nine bands on either side of half-intersection, subtract the difference; within nine bands on either side of true conjunction, add the difference. This adjustment shifts latitude by six degrees—the value compared directly with the ecliptic alone. Compared with the equator, it varies with the seasons and is not constant. Count hou elapsed since the Winter or Summer Solstice, multiply the ecliptic difference, and divide by eighteen to obtain the lunar equatorial latitude difference. For the sun, inside the equator is yin and outside is yang; for the moon, inside the ecliptic is yin and outside is yang. Hence after the spring-equinox crossing the moon follows yin months, and after the autumn-equinox crossing yang months — both are same-named. If after the spring-equinox crossing it follows yang months, or after the autumn-equinox crossing yin months, both are differently named. Under same name, where the difference is for increase, add it; where for decrease, subtract it. Under different name, where the difference is for increase, subtract it; where for decrease, add it. Apply these rules to adjust ecliptic longitude and obtain the fixed nine-path degree.
523
滿 滿
For each central qi, subtract days from mean new moon, add the entered conjunction general term, and subtract from the conjunction cycle to obtain the mean conjunction’s day-count within that qi. Cast out full three-origin intervals; the remainder is the day-count entering the next node. To find the next conjunction, add the conjunction cycle and cast out full three-origin intervals, yielding the next mean conjunction’s day-count within qi.
524
For each qi, apply the initial prior-posterior numbers by addition then subtraction to obtain the mean conjunction’s day-count within fixed qi. Double and multiply by six lines; triple the minor remainder and divide by the chronogram divisor; multiply by that qi’s increase-decrease rate and divide by the fixed-qi chronogram count; use the result to adjust that qi’s anomalistic accumulation as the fixed number.
525
滿 滿退 滿 宿 滿 滿退 滿退宿
Set the mean conjunction’s remainder within fixed qi; add the day’s midnight rotation entry remainder; multiply by that day’s increase-decrease rate, divide by the universal divisor, and adjust that day’s anomalistic accumulation; multiply by the conjunction rate and divide by the conjunction number for the fixed value. Apply the fixed fast-slow numbers for entered qi and rotation—subtract for fast, add for slow—to the mean conjunction’s qi remainder; carry or borrow days to obtain the true conjunction’s day-count within fixed qi. Keep a duplicate of the remainder within fixed qi; multiply by that day’s equation of time, divide by the universal divisor, and add or subtract from the duplicate; add to that night’s midnight solar longitude to obtain the true-conjunction hour-added ecliptic degree. Subtract the true-conjunction hour-added degree remainder from the universal divisor; multiply the remainder by the band index for the true-conjunction lodge’s distance entry to obtain the pre-distance fraction. Take the lunar ecliptic latitude difference for the distance band, multiply by the universal divisor, subtract the pre-distance fraction, and when the remainder fills 240 divide to obtain the fixed difference. If it does not fill, retreat one place for seconds. Add the fixed difference and seconds to the ecliptic degree and remainder; still count hou from the Winter or Summer Solstice, multiply the fixed difference, and divide by eighteen; apply the result according to same or different name; carry or borrow degrees to obtain the true-conjunction hour-added lunar nine-path lodge longitude.
526
宿 宿宿宿 宿 宿滿
Set the hour-added solar degree for each fixed syzygy and accumulate along the nine paths in sequence. At conjunction hour-addition the moon lies hidden beneath the sun at the same longitude—the departure image. Set the ecliptic solar degree at hour-added new, quarter, or full moon; subtract the ecliptic lodge degree at true-conjunction hour-addition; add the remainder to the nine-path lodge at true conjunction; count outward from that lodge to obtain the nine-path longitude at hour-added syzygy. At conjunction hour-addition, if not true conjunction, the sun remains on the ecliptic and the moon on the nine paths; though lodge longitudes differ, their polar distances align to the plumb line. Hence: the moon moves hidden beneath the sun at the same longitude. One image interval: 91°, remainder 954, 22½ seconds—first quarter, Duì ☱. Double it and oppose the sun to obtain full moon, Kǎn ☵. Triple it to obtain last quarter, Zhèn ☳. Add each to the corresponding nine-path lodge; carry seconds into the image cycle and remainder into degrees via the universal divisor to obtain that day’s hour-added lunar longitude. The five positions sum to forty; reduce the degree remainder thereby for parts. The remainder becomes minor parts.
527
退 退 滿
Inspect midnight rotation entry at mean new moon; if the fixed new-moon major remainder advances or retreats, adjust the rotation day likewise. Otherwise take mean new moon as the fixed value. Add one day at each step to obtain the next day. Multiply each midnight rotation entry remainder by the column decline and divide by the universal divisor; use the result to advance or retreat that day’s rotation parts, yielding the lunar rotation fixed parts. When the parts fill the rotation divisor, they become degrees.
528
退
At fixed syzygy midnight rotation entry, halve the column decline and subtract from rotation parts. If retreating, multiply the fixed remainder by the decline, divide by the universal divisor, and halve together with the decline; if advancing, halve the remainder, multiply by the decline, divide by the universal divisor likewise, and add to the amount subtracted. Multiply by the fixed remainder; divide by the universal divisor and subtract from the hour-added lunar degree to obtain midnight lunar longitude. Add the daily rotation fixed parts at each step to obtain the next day. Multiply the entered rotation fixed parts by the day-night clepsydra and divide by double the hundred marks for dawn parts. Subtract from the rotation fixed parts; the remainder is dusk parts. Before full moon add dusk parts, after full moon add dawn parts to midnight longitude to obtain dawn and dusk lunar positions.
529
Intersection day
530
Latitude bend-stretch rates
531
Latitude bend-stretch accumulation
532
Day 1
533
Bend rate: 27
534
Accumulation, initial
535
Day 2
536
Bend rate: 19
537
Accumulation: 27
538
Day 3
539
Bend rate: 13
540
Accumulation: 46
541
Day 4
542
Bend rate: 8
543
Accumulation: 59
544
Day 5
545
Bend rate: 13
546
Accumulation: 67
547
Day 6
548
Bend rate: 19
549
Accumulation: 1° 4
550
Day 7
551
Initial bend rate: 20, terminal stretch rate: 7
552
Accumulation: 1° 23
553
Day 8
554
Stretch rate: 19
555
Accumulation: 1° 36
556
Day 9
557
Stretch rate: 13
558
Accumulation: 1° 17
559
Day 10
560
Stretch rate: 8
561
Accumulation: 1° 4
562
Day 11
563
Stretch rate: 13
564
Accumulation: 72
565
Day 12
566
Stretch rate: 19
567
Accumulation: 59
568
Day 13
569
Stretch rate: 27
570
Accumulation: 40
571
Day 14
572
Initial stretch rate: 13, terminal bend rate enters thereafter
573
Accumulation: 13
574
宿
For each day, take the yin-yang month intersection-day count at midnight; where the moon-path and ecliptic are same-named, add the bend-stretch accumulation below; where differently named, subtract it. Apply these adjustments to each day’s dawn and dusk ecliptic lunar longitudes to obtain fixed lodge degrees and parts.
575
V. Method for Determining Orbital Clepsydra
576
Line cycle: 1,520
577
Image accumulation: 480.
578
Chronogram interval: 8 ke, 160 fen.
579
Twilight interval: 2 ke, 240 fen.
580
Fixed qi
581
Rates of ascension and descent
582
Message wane
583
Yangcheng gnomon table
584
Clepsydra marks
585
Ecliptic polar distance
586
Distance to culminating star
587
Winter Solstice
588
Descent rate: 78
589
Message wane: void 64
590
Gnomon shadow: 1 zhang 2 chi 7 cun 1 fen 50
591
27 ke 230 fen
592
117° 20 parts
593
82° 26 parts
594
Lesser Cold
595
Descent rate: 72
596
Message wane: 11, 91
597
Gnomon shadow: 1 zhang 2 chi 2 cun 2 fen 77
598
27 ke 135 fen
599
114° 35 parts
600
82° 91 parts
601
Greater Cold
602
Descent rate: 53
603
Message wane: 22, 42
604
Gnomon shadow: 1 zhang 1 chi 2 cun 1 fen 82
605
26 ke 380 fen
606
111° 90 parts
607
84° 77 parts
608
Start of Spring
609
Descent rate: 34
610
Message wane: 30, 25
611
Gnomon shadow: 9 chi 7 cun 3 fen 51
612
25 ke 475 fen
613
108° 5 parts
614
87° 70 parts
615
Rain Water
616
Descent, initial limit: 78
617
Message wane: 35, 78
618
Gnomon shadow: 8 chi 2 cun 1 fen 6
619
24 ke 470 fen
620
103° 20 parts
621
91° 39 parts
622
Awakening of Insects
623
Descent rate: 1
624
Message wane: 39, 50
625
Gnomon shadow: 6 chi 7 cun 3 fen 84
626
23 ke 360 fen
627
97° 30 parts
628
95° 88 parts
629
Spring Equinox
630
Ascension rate: 5
631
Message wane: 39, 65
632
Gnomon shadow: 5 chi 4 cun 3 fen 19
633
22 ke 230 fen
634
91° 30 parts
635
100° 44 parts 50
636
Pure Brightness
637
Ascension, initial limit: 1
638
Message wane: 38, 89
639
Gnomon shadow: 4 chi 3 cun 2 fen 11
640
21 ke 120 fen
641
85° 30 parts
642
105° 1 parts
643
Grain Rain
644
Ascension rate: 32
645
Message wane: 33, 56
646
Gnomon shadow: 3 chi 3 cun 47
647
20 ke 10 fen
648
79° 30 parts
649
109° 50 parts
650
Start of Summer
651
Ascension rate: 52
652
Message wane: 28, 38
653
Gnomon shadow: 2 chi 5 cun 3 fen 31
654
19 ke 5 fen
655
74° 55 parts
656
113° 19 parts
657
滿
Lesser Fullness
658
Ascension rate: 63
659
Message wane: 20, 12
660
Gnomon shadow: 1 chi 9 cun 5 fen 76
661
18 ke 100 fen
662
70° 70 parts
663
116° 12 parts
664
Grain in Ear
665
Ascension rate: 64
666
Message wane: 10, 12
667
Gnomon shadow: 1 chi 6 cun 3
668
17 ke 335 fen
669
68° 25 parts
670
117° 98 parts
671
Summer Solstice
672
Descent rate: 64
673
Wane: void 52
674
Gnomon shadow: 1 chi 4 cun 7 fen 79
675
17 ke 250 fen
676
67° 40 parts
677
118° 63 parts
678
Lesser Heat
679
Descent rate: 63
680
Wane: 17, 16
681
Gnomon shadow: 1 chi 6 cun 3
682
17 ke 335 fen
683
68° 25 parts
684
117° 98 parts
685
Greater Heat
686
Descent rate: 52
687
Wane: 27, 15
688
Gnomon shadow: 1 chi 9 cun 5 fen 76
689
18 ke 100 fen
690
70° 70 parts
691
116° 12 parts
692
Start of Autumn
693
Descent rate: 32
694
Wane: 28, 90
695
Gnomon shadow: 2 chi 5 cun 3 fen 31
696
19 ke 5 fen
697
74° 55 parts
698
113° 19 parts
699
End of Heat
700
Descent, initial limit: 99
701
Wane: 34, 55
702
Gnomon shadow: 3 chi 3 cun 47
703
20 ke 10 fen
704
79° 30 parts
705
109° 50 parts
706
White Dew
707
Descent rate: 5
708
Wane: 38, 90
709
Gnomon shadow: 4 chi 3 cun 2 fen 11
710
21 ke 120 fen
711
85° 30 parts
712
105° 1 parts
713
Autumn Equinox
714
Ascension rate: 1
715
Wane: 39, 66
716
Gnomon shadow: 5 chi 4 cun 3 fen 19
717
22 ke 230 fen
718
91° 30 parts
719
100° 44 parts 50
720
Cold Dew
721
Ascension, initial limit: 1
722
Wane: 39, 50
723
Gnomon shadow: 6 chi 7 cun 3 fen 84
724
23 ke 360 fen
725
97° 30 parts
726
95° 88 parts
727
Frost Descent
728
Ascension rate: 34
729
廿
Wane: 24, 98
730
Gnomon shadow: 8 chi 2 cun 1 fen 6
731
24 ke 470 fen
732
103° 20 parts
733
91° 39 parts
734
Start of Winter
735
Ascension rate: 53
736
Wane: 29, 72
737
Gnomon shadow: 9 chi 7 cun 3 fen 51
738
25 ke 475 fen
739
108° 5 parts
740
87° 70 parts
741
Lesser Snow
742
Ascension rate: 72
743
Wane: 21, 70
744
Gnomon shadow: 1 zhang 1 chi 2 cun 1 fen 82
745
26 ke 380 fen
746
111° 90 parts
747
84° 77 parts
748
Greater Snow
749
Ascension rate: 78
750
Wane: 11, 13
751
Gnomon shadow: 1 zhang 2 chi 2 cun 2 fen 77
752
27 ke 135 fen
753
114° 35 parts
754
82° 91 parts
755
滿
For each seasonal node, set its message-wane constant; for each day in that fixed qi, apply the ascension-descent rate—subtract on ascension, add on descent—to the parts; carry hundreds into the wane tally to obtain the daily fixed message wane. Outside the single qi bracketing each equinox, where ascension and descent are unequal, a three-day band limit applies throughout. Rain Water, day 1: descent rate 78. First band: decrease 12 per day. Second band: decrease 8 per day. Third band: decrease 3 per day. Fourth band: decrease 2 per day. Fifth band: decrease 1 per day. Pure Brightness, day 1: ascension rate 1. First band: increase 1 per day. Second band: increase 2 per day. Third band: increase 3 per day. Fourth band: increase 8 per day. Final band: increase 19 per day. End of Heat, day 1: descent rate 99. First band: decrease 19 per day. Second band: decrease 8 per day. Third band: decrease 3 per day. Fourth band: decrease 2 per day. Final band: decrease 1 per day. Cold Dew, day 1: ascension rate 1. First band: increase 1 per day. Second band: increase 2 per day. Third band: increase 3 per day. Fourth band: increase 8 per day. Final band: increase 12 per day. Set each first-day ascension-descent rate; step through the limit bands by increase or decrease to obtain the daily rate. Then successively subtract ascension and add descent from the qi’s opening message wane to obtain the daily fixed wane.
756
滿
Directly beneath the sub-solar point in the south, at true noon there is no shadow. One degree north of the sub-solar point, the initial count is 1,379. From here the increment begins: add 1 per degree up to 25°, for a total increase of 26 parts. Then add 2 per degree up to 40°. Then add 6 per degree up to 44°, increase 68. Then add 2 per degree up to 50°. Then add 7 per degree up to 55°. Then add 19 per degree up to 60°, increase 160. Then add 33 per degree up to 65°. Then add 36 per degree up to 70°. Then add 39 per degree up to 72°, increase 260. Then add 440 per degree. Then add 1,060 per degree. Then add 1,860 per degree. Then add 2,840 per degree. Then add 4,000 per degree. Then add 5,340 per degree. Each value is the per-degree difference. Sum the differences cumulatively onto the initial count; carry hundreds into parts and tens of parts into cun to obtain the per-degree gnomon difference. Sum those differences again to obtain the gnomon reading for each degree north of the sub-solar point.
757
滿
Set the qi’s polar distance and subtract 56° 82½ parts (the pole’s offset from the sub-solar point) to obtain degrees north of the sub-solar point. Take the per-degree gnomon difference at the degree of the fixed message wane; carry hundreds into parts and tens into cun for the daily gnomon difference. Then successively subtract on waning breath and add on growing breath from the qi’s opening gnomon count to obtain the daily mean noon gnomon constant.
758
Take the day’s fixed minor remainder within its qi, subtract the line divisor, and the remainder is the after-noon fraction. If it will not subtract, reverse the subtraction to obtain the before-noon fraction. Multiply by the gnomon difference, divide by the universal divisor, and obtain the variation difference. Apply it to the mean noon gnomon constant: after Winter Solstice, subtract before noon and add after noon. After Summer Solstice, add before noon and subtract after noon. On Winter Solstice day, only decrease applies—no increase. On Summer Solstice day, only increase applies—no decrease. This yields the daily fixed noon gnomon count.
759
滿滿
Set the fixed message wane again; carry image accumulation into clepsydra marks, leaving the remainder as parts. Successively subtract on waning breath and add on growing breath from the qi’s opening midnight leak to obtain the daily fixed midnight leak. For whole marks, multiply by 9,120, add 19 times the fractional marks, divide by 300, and obtain the dawn-opening remainder.
760
Double the midnight leak to obtain night clepsydra marks. Subtract from 100 marks; the remainder is day marks. Move five marks from day to night: day marks become appearance marks, night marks disappearance marks. Add half disappearance marks to half a chronogram; count outward from the zi-opening tally to obtain sunrise chronogram marks. Add appearance marks and assign the count to obtain sunset. Set night marks, divide by five, and obtain the per-watch mark difference. Divide by five again for the per-stave mark difference. Add dusk marks to the sunset chronogram mark to obtain the first watch of night A. Add the watch-stave difference repeatedly to obtain the chronogram for each watch and stave of the five night watches. The fixed midnight leak is also called dawn-opening night marks.
761
滿滿
Set the fixed message wane again; carry hundreds into degrees, leaving the remainder as parts. Successively subtract on waning breath and add on growing breath from the qi’s opening polar distance to obtain the daily fixed polar distance.
762
滿
Set the fixed message wane, multiply by 12,386, divide by 16,277, and obtain the degree difference. When the difference fills 100, carry into degrees. Successively add on waning breath and subtract on growing breath from the qi’s opening distance to culmination to obtain the daily fixed culminating distance. Double it, subtract from the circuit of heaven, and obtain the distance from zi.
763
Take the day’s equatorial solar longitude, add culminating distance, and obtain the dusk culminating star. Double the distance from zi, add to the dusk star, and obtain the dawn culminating star. Take the dusk culminating star as night A’s culminating star; add the per-watch degree difference for each of the five night watches.
764
使
Across the nine domains, the mean noon gnomon constants at each qi’s opening are not uniform. Subtract each qi’s polar distances pairwise; each difference is that qi’s fixed message count. Measure the locality’s solstitial gnomon; one solstice suffices—both winter and summer need not be taken. Among per-degree gnomon counts north of the sub-solar point, match equal shadow lengths to fix that place’s degrees and parts north of the sub-solar point. For each qi, apply its fixed message count; after Winter Solstice, subtract for each qi. After Summer Solstice, add for each qi. This yields each qi’s degrees north of the sub-solar point. Take the gnomon count at each degree and part as that locality’s fixed mean noon gnomon constant at each qi’s opening. If the measured shadow falls south of the table, match its length to the north-of-sub-solar per-degree table, take the corresponding degree, and subtract from degrees north of the sub-solar point. Reverse the sign to obtain degrees south of the sub-solar point. Then apply the fixed message count by addition or subtraction.
765
At each solstice, calibrate the local water clock to fix the day-and-night clepsydra marks for that place. Subtract the two to obtain the solstitial mark difference. Halve the difference and apply it to the solstitial day-night marks to fix the spring and autumn equinox opening day-night marks. Then set each qi’s fixed message count. Multiply by the local mark difference, divide by the solstitial polar-distance span (47 parts 80), and add or subtract the opening day-night leak marks by fractional rank to obtain each remaining fixed qi’s opening day-night leaks.
766
滿
Take the daily fixed message wane, multiply by the mark difference, divide by the degree difference, and step the qi’s opening leaks by waning breath and growing breath to obtain the next day. Distance to culmination, dusk and dawn culminating stars, and sunrise and sunset are all found by the Yangcheng method. Multiply by the mark difference and divide by the degree difference for the present-part correction. Match the locality’s fixed equinox mean noon gnomon to Yangcheng’s daily table; on the matching day, its midnight leak becomes the locality’s fixed equinox opening midnight leak. For each remaining fixed qi’s opening day, apply the fixed message count to marks and parts by fractional rank—subtract after spring equinox, add after autumn equinox. Carry image accumulation into clepsydra marks. For the next day, step the fixed message wane by the Yangcheng procedure. This method plumbs the principle and is broadly sound. Yet mountain heights and level plains do not present the sun equally. Only when their noon shadows are compared do lengths agree. Water-clock flows differ greatly in rate. On this comparison, the earlier method is the more reliable.
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